[ { "key": "X3P8UMS4", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/X3P8UMS4", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/X3P8UMS4", "type": "text/html" }, "up": { "href": "https://api.zotero.org/groups/420663/items/CDJNNXMS", "type": "application/json" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } } }, "data": { "key": "X3P8UMS4", "version": 2, "parentItem": "CDJNNXMS", "itemType": "attachment", "linkMode": "linked_url", "title": "Google Books Link", "accessDate": "2015-10-19T22:24:13Z", "url": "https://books.google.com/books?id=WWjuCAAAQBAJ", "note": "", "contentType": "text/html", "charset": "", "tags": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "RUHPM2R2", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/RUHPM2R2", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/RUHPM2R2", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Chen et al.", "parsedDate": "2013-02-04", "numChildren": 0 }, "data": { "key": "RUHPM2R2", "version": 2, "itemType": "journalArticle", "title": "Performance and uncertainty evaluation of empirical downscaling methods in quantifying the climate change impacts on hydrology over two North American river basins", "creators": [ { "creatorType": "author", "firstName": "Jie", "lastName": "Chen" }, { "creatorType": "author", "firstName": "François P.", "lastName": "Brissette" }, { "creatorType": "author", "firstName": "Diane", "lastName": "Chaumont" }, { "creatorType": "author", "firstName": "Marco", "lastName": "Braun" } ], "abstractNote": "Summary\nStatistical and dynamical downscaling techniques have been proposed to bridge the gaps between coarse-scale and generally biased climate model outputs and the point-scale requirements of impact model inputs. Amongst the various statistical approaches, empirical downscaling methods are the most commonly used due to their ease of implementation. Several empirical downscaling approaches have been proposed and need to be assessed as to which method contributes (or not) to the overall climate change uncertainty. Accordingly, this work aims at assessing the uncertainty of six empirical downscaling methods in quantifying the hydrological impact of climate change over two North American river basins under different climate conditions. The six empirical downscaling methods are grouped into change factor (two methods) and bias correction (four methods) approaches. The uncertainty related to the choice of an empirical downscaling method is compared to that associated with the choice of climate simulation, through the use of two Regional Climate Models (RCMs) driven by three different General Circulation Models (GCMs), totaling four RCM simulations, taken from the NARCCAP inter-comparison project. The future (2041–2065) hydrological regimes simulated with an empirical lumped hydrology model (HSAMI) are compared to the reference period (1971–1995) using a set of hydrology criteria which includes statistics of both mean and extreme values. The results show a large uncertainty envelope associated with the choice of a given empirical downscaling method, as well as for the choice of an RCM simulation. The uncertainty due to empirical downscaling and RCM simulation was more significant in projecting extreme streamflow than in projecting mean flows. Comparing the uncertainty envelope of empirical downscaling methods to the envelope resulting from four RCM simulations indicates that both are similar, even though the latter was slightly larger for some statistics. Finally, the uncertainty linked to the choice of an empirical downscaling approach (change factor vs. bias correction) was much larger than within each type. Overall, this work emphasizes the importance of using several climate projections and empirical downscaling approaches to delineate uncertainty when assessing the climate change impacts on hydrology.", "publicationTitle": "Journal of Hydrology", "publisher": "", "place": "", "date": "February 4, 2013", "volume": "479", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "200-214", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Journal of Hydrology", "DOI": "10.1016/j.jhydrol.2012.11.062", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S0022169412010414", "accessDate": "2015-10-23T17:31:03Z", "PMID": "", "PMCID": "", "ISSN": "0022-1694", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Climate Change", "type": 1 }, { "tag": "Empirical downscaling", "type": 1 }, { "tag": "Hydrology", "type": 1 }, { "tag": "Model output statistics", "type": 1 }, { "tag": "Uncertainty", "type": 1 } ], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "UHDZR99B", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/UHDZR99B", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/UHDZR99B", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Hambright et al.", "parsedDate": "2000", "numChildren": 0 }, "data": { "key": "UHDZR99B", "version": 2, "itemType": "journalArticle", "title": "Indices of water quality for sustainable management and conservation of an arid region lake, Lake Kinneret (Sea of Galilee), Israel", "creators": [ { "creatorType": "author", "firstName": "K. David", "lastName": "Hambright" }, { "creatorType": "author", "firstName": "Arkady", "lastName": "Parparov" }, { "creatorType": "author", "firstName": "Tom", "lastName": "Berman" } ], "abstractNote": "", "publicationTitle": "Aquatic Conservation Marine and Freshwater Ecosystems", "publisher": "", "place": "", "date": "2000", "volume": "10", "issue": "6", "section": "", "partNumber": "", "partTitle": "", "pages": "393-406", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1002/1099-0755(200011/12)10:63.3.CO;2-F", "citationKey": "", "url": "http://www.researchgate.net/publication/233792804_Indices_of_water_quality_for_sustainable_management_and_conservation_of_an_arid_region_lake_Lake_Kinneret_%28Sea_of_Galilee%29_Israel", "accessDate": "", "PMID": "", "PMCID": "", "ISSN": "1099-0755", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "8VTB7S6C", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/8VTB7S6C", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/8VTB7S6C", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Nicholson", "parsedDate": "1999-01", "numChildren": 0 }, "data": { "key": "8VTB7S6C", "version": 2, "itemType": "journalArticle", "title": "Historical and Modern Fluctuations of Lakes Tanganyika and Rukwa and Their Relationship to Rainfall Variability", "creators": [ { "creatorType": "author", "firstName": "Sharon E.", "lastName": "Nicholson" } ], "abstractNote": "This paper describes the fluctuations of Lakes Tanganyika and Rukwa over the last two centuries. Lake chronologies extending back to the late eighteenth century are derived from reports of European visitors, settlers and explorers and from oral accounts of the local peoples. The historical fluctuations are meshed with the modern record to provide a picture of the lakes' fluctuations until the late twentieth century. The historical fluctuations of the lakes are quite similar. The most important of these are low levels during the first half of the nineteenth century, very high stands in the last decades of the nineteenth century, and, around the turn of the century, a rapid fall to twentieth century levels. This pattern is ubiquitous throughout eastern Africa and is apparent in numerous other lakes, including Victoria, Naivasha, Stefanie, Turkana, Malawi and Chilwa. Driest periods were in the 1920s or earlier and in the 1950s. Lake Tanganyika returned to extremely high stands in the 1960s and has continued to maintain relatively high stands since that time. Lake Rukwa rose to high stands during the 1980s and maintained them for several years. An analysis of rainfall variability shows that these trends are generally explained by variations in catchment rainfall. However, the lakes' responses to rainfall variability are sometimes dissimilar because Lake Rukwa is a closed basin. Our results demonstrate the complexity of the rainfall/lake-level relationships and the need to use water balance relationships in order to interpret the lakes' historical or paleo-fluctuations in terms of rainfall.", "publicationTitle": "Climatic Change", "publisher": "", "place": "", "date": "1999-01", "volume": "41", "issue": "1", "section": "", "partNumber": "", "partTitle": "", "pages": "53-71", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Climatic Change", "DOI": "10.1023/A:1005424619718", "citationKey": "", "url": "http://link.springer.com/article/10.1023/A%3A1005424619718", "accessDate": "2015-10-20T21:11:29Z", "PMID": "", "PMCID": "", "ISSN": "0165-0009, 1573-1480", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "en", "libraryCatalog": "link.springer.com", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Meteorology/Climatology", "type": 1 } ], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "4RDBMQBG", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/4RDBMQBG", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/4RDBMQBG", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Lazar et al.", "parsedDate": "2008-07-15", "numChildren": 0 }, "data": { "key": "4RDBMQBG", "version": 2, "itemType": "journalArticle", "title": "Ra and Th adsorption coefficients in lakes—Lake Kinneret (Sea of Galilee) “natural experiment”", "creators": [ { "creatorType": "author", "firstName": "Boaz", "lastName": "Lazar" }, { "creatorType": "author", "firstName": "Yishai", "lastName": "Weinstein" }, { "creatorType": "author", "firstName": "Adina", "lastName": "Paytan" }, { "creatorType": "author", "firstName": "Einat", "lastName": "Magal" }, { "creatorType": "author", "firstName": "Debbie", "lastName": "Bruce" }, { "creatorType": "author", "firstName": "Yehoshua", "lastName": "Kolodny" } ], "abstractNote": "The adsorption rate constants of Ra and Th were estimated from empirical data from a freshwater lake and its feeding saline springs. We utilized the unique setting of Lake Kinneret (Sea of Galilee, northern Israel) in which most of the Ra and Th nuclides are introduced into the lake by saline springs with high 226Ra activities and a high 224Ra/228Ra ratio of 1.5. The mixing of the Ra enriched saline waters and freshwater in the lake causes the 224Ra/228Ra ratio to drop down to 0.1 in the Kinneret due to preferential adsorption of 228Th. These conditions constitute a “natural experiment” for estimating adsorption rates. We developed a simple mass-balance model for the radionuclides in Lake Kinneret that accurately predicted the Ra isotope ratios and the 226Ra activity in the lake. The model is comprised of simultaneous equations; one for each radionuclide. The equations have one input term: supply of radionuclides from the saline springs; and three output terms: adsorption on particles in the lake, radioactive decay and outflow from the lake. The redundancy in the analytical solutions to the mass balance equations for the relevant nuclides constrained the values of Ra and Th adsorption rate constants to a very narrow range. Our results indicate that the adsorption rate constant for Ra is between 0.005 d−1 and 0.02 d−1. The rate constant for Th is between 0.5 d−1 and 1 d−1, about fifty to a hundred times higher. The estimated desorption rate coefficient for Ra is about 50–100 times larger than its adsorption rate constant. The mass-balance equations show that the residence times of all Ra isotopes (226Ra, 228Ra,223Ra, 224Ra) and of 228Th in the lake are about 95, 92, 14, 6 and 1 d, respectively. These residence times are much shorter than the residence time of water in the lake (about 5.5 y). The steady state activity ratios in Lake Kinneret depend mainly on the adsorption rate constants, decay constants, the outflow rate from the lake and the activity ratios in the saline springs. The activity ratios are independent of the saline springs flow rate.", "publicationTitle": "Geochimica et Cosmochimica Acta", "publisher": "", "place": "", "date": "July 15, 2008", "volume": "72", "issue": "14", "section": "", "partNumber": "", "partTitle": "", "pages": "3446-3459", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Geochimica et Cosmochimica Acta", "DOI": "10.1016/j.gca.2008.02.027", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S0016703708002561", "accessDate": "2015-10-23T16:28:08Z", "PMID": "", "PMCID": "", "ISSN": "0016-7037", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "SM6Z5B22", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/SM6Z5B22", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/SM6Z5B22", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Dumont", "parsedDate": "1998-01-01", "numChildren": 0 }, "data": { "key": "SM6Z5B22", "version": 2, "itemType": "journalArticle", "title": "The Caspian Lake: History, biota, structure, and function", "creators": [ { "creatorType": "author", "firstName": "H. J.", "lastName": "Dumont" } ], "abstractNote": "The elongate, endorheic Caspian Lake has a north-south orientation and its main freshwater inflow, the Volga River, enters at the shallow north end. Two deep basins occupy its central and southern regions. These facts lead to horizontal differences in temperature, salinity, and ecology. Nutrient levels and primary production are low. Historically, lake level has fluctuated by ~6 m, but on the geological timescale, fluctuations of >200 m have occurred. The lake formed in the late Miocene, first went through a long shrinking phase, expanded to three times its present size in the late Pliocene, and repeatedly rose and fell throughout the Pleistocene, with corresponding freshenings and salinizations. The lake surface has remained below sea level since the last pleniglacial. This dynamic history led to the assemblage of a set of euryhaline biota of Tethyan and freshwater origin, besides Baltic elements, that invaded with glacial meltwater. Endemism is as high as in Lake Baikal, but typical marine groups are absent. Because the lake is oxygenated to the bottom, its biota show a vertical zonation, but without a true abyssal community, suggesting catastrophic episodes of deep anoxia.", "publicationTitle": "Limnology and Oceanography", "publisher": "", "place": "", "date": "January 1, 1998", "volume": "43", "issue": "1", "section": "", "partNumber": "", "partTitle": "", "pages": "44-52", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Limnol. Oceanogr.", "DOI": "10.4319/lo.1998.43.1.0044", "citationKey": "", "url": "http://onlinelibrary.wiley.com/doi/10.4319/lo.1998.43.1.0044/abstract", "accessDate": "2015-10-19T22:31:49Z", "PMID": "", "PMCID": "", "ISSN": "1939-5590", "archive": "", "archiveLocation": "", "shortTitle": "The Caspian Lake", "language": "en", "libraryCatalog": "Wiley Online Library", "callNumber": "", "rights": "© 1998, by the Association for the Sciences of Limnology and Oceanography, Inc.", "extra": "", "tags": [], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "CDJNNXMS", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/CDJNNXMS", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/CDJNNXMS", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Dejoux", "parsedDate": "2012-12-06", "numChildren": 1 }, "data": { "key": "CDJNNXMS", "version": 2, "itemType": "book", "title": "Lake Titicaca: A Synthesis of Limnological Knowledge", "creators": [ { "creatorType": "author", "firstName": "C.", "lastName": "Dejoux" } ], "abstractNote": "Lake Titicaca, because of its area and volume and its situation at high attitude within the tropics, is a unique hydrological site in the world. It should be noted that it stands at the transition point between two very distinct geographical regions: the desert fringe of the Pacific coast to the west and the great Amazonian forest extending to the Atlantic coast to the east. Many scientists have been attracted to the lake in the past because of its unusual limnological features. In this book the editors have compiled an exhaustive review of current knowledge from the existing literature and from the results of more recent observations. It is certain that this book will become the essential reference work for scientists wanting to make progress in revealing the lake's secrets. It can be stated unequivocally that this work constitutes a complete review of the present state of knowledge on Lake Titicaca and that it provides the latest results of research on this habitat.", "series": "", "seriesNumber": "", "volume": "", "numberOfVolumes": "", "edition": "", "date": "2012-12-06", "publisher": "Springer Science & Business Media", "place": "", "originalDate": "", "originalPublisher": "", "originalPlace": "", "format": "", "numPages": "606", "ISBN": "978-94-011-2406-5", "DOI": "", "citationKey": "", "url": "", "accessDate": "", "ISSN": "", "archive": "", "archiveLocation": "", "shortTitle": "Lake Titicaca", "language": "en", "libraryCatalog": "Google Books", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Science / Life Sciences / Ecology", "type": 1 } ], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "2WGAIC2M", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/2WGAIC2M", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/2WGAIC2M", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Bradbury et al.", "parsedDate": "1981-12-18", "numChildren": 0 }, "data": { "key": "2WGAIC2M", "version": 2, "itemType": "journalArticle", "title": "Late Quaternary Environmental History of Lake Valencia, Venezuela", "creators": [ { "creatorType": "author", "firstName": "J. Platt", "lastName": "Bradbury" }, { "creatorType": "author", "firstName": "B.", "lastName": "Leyden" }, { "creatorType": "author", "firstName": "M.", "lastName": "Salgado-Labouriau" }, { "creatorType": "author", "firstName": "W. M.", "lastName": "Lewis" }, { "creatorType": "author", "firstName": "C.", "lastName": "Schubert" }, { "creatorType": "author", "firstName": "M. W.", "lastName": "Binford" }, { "creatorType": "author", "firstName": "D. G.", "lastName": "Frey" }, { "creatorType": "author", "firstName": "D. R.", "lastName": "Whitehead" }, { "creatorType": "author", "firstName": "F. H.", "lastName": "Weibezahn" } ], "abstractNote": "Chemical, paleontological, and mineralogical analyses of a 7.5-meter core from the middle of Lake Valencia, Venezuela, have provided information on the paleoclimatic history of this low-elevation, low-latitude site for the last 13,000 years. The data show that dry climates existed in this region from 13,000 years before present (B.P.) until about 10,000 years B.P. The Lake Valencia Basin was occupied by intermittent saline marshes at that time. About 10,000 years B.P., a permanent lake of fluctuating salinity formed and arboreal plant communities replaced the earlier dominant xeric herbaceous vegetation and marsh plants. By 8500 years B.P., Lake Valencia reached moderate to low salinities and discharged water; the modern vegetation became established at that time. After 8500 years B.P., the lake twice ceased discharging as a result of reduced watershed moisture. The second of these drying episodes is still in progress and has been aggravated by human activities in the watershed.", "publicationTitle": "Science", "publisher": "", "place": "", "date": "December 18, 1981", "volume": "214", "issue": "4527", "section": "", "partNumber": "", "partTitle": "", "pages": "1299-1305", "series": "New Series", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Science", "DOI": "", "citationKey": "", "url": "http://www.jstor.org/stable/1687836", "accessDate": "2015-10-19T22:12:33Z", "PMID": "", "PMCID": "", "ISSN": "0036-8075", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "JSTOR", "callNumber": "", "rights": "Copyright © 1981 American Association for the Advancement of Science", "extra": "", "tags": [], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "AHFZ8B8P", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/AHFZ8B8P", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/AHFZ8B8P", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Sidle et al.", "parsedDate": "2007-02-13", "numChildren": 0 }, "data": { "key": "AHFZ8B8P", "version": 2, "itemType": "journalArticle", "title": "Contemporary changes in open water surface area of Lake Inle, Myanmar", "creators": [ { "creatorType": "author", "firstName": "Roy C.", "lastName": "Sidle" }, { "creatorType": "author", "firstName": "Alan D.", "lastName": "Ziegler" }, { "creatorType": "author", "firstName": "John B.", "lastName": "Vogler" } ], "abstractNote": "From 1935 to 2000, the net open water area of Inle Lake in Central Shan State, Myanmar decreased from 69.10 to 46.69 km2, a loss of 32.4% during this 65-year period. Local beliefs are that losses in lake area have been even greater within the last 100–200 years. Various activities, including timber removal, shifting agriculture in the uplands by various ethnic groups, and unsustainable cultivation practices on the low- and mid-level hillslopes around the lake, have been blamed for both historical and ongoing sedimentation. We take issue with attributing loss of lake area to these activities, and propose instead that ongoing “in-lake” and “near-lake” agricultural practices are the main sources of contemporary sediment and loss of open water area. About 93% (i.e., 20.84 km2) of the recent loss in open water area of the lake is due to the development of floating garden agriculture, largely along the west side of the lake. Direct environmental impacts associated with this practice and with other agriculture activities within the wetlands and margins of the lake include sedimentation, eutrophication, and pollution. Whilst the sustainability of hillslope agriculture and past forestry practices can indeed be questioned, a more urgent need is to address these \"in-lake\" and \"near-lake\" practices.", "publicationTitle": "Sustainability Science", "publisher": "", "place": "", "date": "2007/02/13", "volume": "2", "issue": "1", "section": "", "partNumber": "", "partTitle": "", "pages": "55-65", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Sustain Sci", "DOI": "10.1007/s11625-006-0020-7", "citationKey": "", "url": "https://courses.nus.edu.sg/course/geoadz/internet/publications/Sidle%20et%20al%202007_SustainSci_Inle%20Lake%20Myanmar.pdf", "accessDate": "2015-10-20T19:49:25Z", "PMID": "", "PMCID": "", "ISSN": "1862-4065, 1862-4057", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "en", "libraryCatalog": "link.springer.com", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Climate Change", "type": 1 }, { "tag": "Deforestation", "type": 1 }, { "tag": "Environmental Economics", "type": 1 }, { "tag": "Environmental Management", "type": 1 }, { "tag": "Erosion", "type": 1 }, { "tag": "Floating gardens", "type": 1 }, { "tag": "Landscape Ecology", "type": 1 }, { "tag": "Public Health/Gesundheitswesen", "type": 1 }, { "tag": "Sedimentation", "type": 1 }, { "tag": "Shifting cultivation", "type": 1 }, { "tag": "Tourism", "type": 1 } ], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "VQJSSDQQ", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/VQJSSDQQ", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/VQJSSDQQ", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Habeck-Fardy and Nanson", "parsedDate": "2014-05", "numChildren": 0 }, "data": { "key": "VQJSSDQQ", "version": 2, "itemType": "journalArticle", "title": "Environmental character and history of the Lake Eyre Basin, one seventh of the Australian continent", "creators": [ { "creatorType": "author", "firstName": "Anna", "lastName": "Habeck-Fardy" }, { "creatorType": "author", "firstName": "Gerald C.", "lastName": "Nanson" } ], "abstractNote": "One of the world's largest internally drained (endorheic) basins, the 1.14 million km2 Lake Eyre (hydrological) Basin (LEB), covers nearly 15% of the Australian continent. Palaeoclimatic and associated flow regime variations are recorded in an archive of fluvial, aeolian and lacustrine sediments that are particularly accessible for deposits from the past ~ 300 ka, and are especially relevant for the past ~ 50 ka during which humans have inhabited Australia. Due to its great size, economic resources and diverse latitudinal extent, it has for over six decades been the focus of environmental, scientific and resource-based studies across numerous disciplines. With an emphasis on assessing the scientific and environmental research over this period, this paper is divided into four parts: Part A provides an introduction and background. Part B provides the geological history, including evidence of substantial Tertiary and Quaternary climate change. Part C covers the contemporary environmental conditions, and Part D presents a conclusion and summary. This not only represents the first comprehensive review of current knowledge of any of the world's truly large dryland drainage basins, but also highlights how more multi-disciplinary research is required. Key remaining questions revolve around the impact of global weather systems on the LEB; the lake-level story in relation to a more precise picture of Late Quaternary climate change; the role of humans and climate in the demise of the megafauna; modern hydrological changes; the role of vegetation in altering channel morphology and flow efficiencies; and nature of flood transmissions.", "publicationTitle": "Earth-Science Reviews", "publisher": "", "place": "", "date": "May 2014", "volume": "132", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "39-66", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Earth-Science Reviews", "DOI": "10.1016/j.earscirev.2014.02.003", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S0012825214000270", "accessDate": "2015-10-19T21:35:57Z", "PMID": "", "PMCID": "", "ISSN": "0012-8252", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Geology", "type": 1 }, { "tag": "Geomorphology", "type": 1 }, { "tag": "Hydrology", "type": 1 }, { "tag": "Lake Eyre Basin", "type": 1 }, { "tag": "Palaeoclimate", "type": 1 } ], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "ZV6PHJ8U", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/ZV6PHJ8U", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/ZV6PHJ8U", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Goulden et al.", "parsedDate": "2002", "numChildren": 0 }, "data": { "key": "ZV6PHJ8U", "version": 2, "itemType": "journalArticle", "title": "Lake Khovsgol: The Blue Pearl of Mongolia", "creators": [ { "creatorType": "author", "firstName": "Clyde E.", "lastName": "Goulden" }, { "creatorType": "author", "firstName": "Jon", "lastName": "Gelhaus" }, { "creatorType": "author", "firstName": "Cully", "lastName": "Hession" }, { "creatorType": "author", "firstName": "B.", "lastName": "Boldgiv" } ], "abstractNote": "", "publicationTitle": "Focus on Geography", "publisher": "", "place": "", "date": "2002", "volume": "47", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "14-19", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "", "accessDate": "", "PMID": "", "PMCID": "", "ISSN": "1549-4934", "archive": "", "archiveLocation": "", "shortTitle": "Lake Khovsgol", "language": "", "libraryCatalog": "", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "5Z5IIZT9", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/5Z5IIZT9", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/5Z5IIZT9", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Romanovsky", "parsedDate": "2012-12-06", "numChildren": 0 }, "data": { "key": "5Z5IIZT9", "version": 2, "itemType": "bookSection", "title": "Water Level Variations and Water Balance of Lake Issyk-Kul", "creators": [ { "creatorType": "author", "firstName": "V.V.", "lastName": "Romanovsky" } ], "abstractNote": "", "bookTitle": "Lake Issyk-Kul: Its Natural Environment", "series": "", "seriesNumber": "", "volume": "", "numberOfVolumes": "", "edition": "", "date": "2012-12-06", "publisher": "Springer Science & Business Media", "place": "", "originalDate": "", "originalPublisher": "", "originalPlace": "", "format": "", "pages": "", "ISBN": "978-94-010-0491-6", "DOI": "", "citationKey": "", "url": "", "accessDate": "", "ISSN": "", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "5VBADES2", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/5VBADES2", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/5VBADES2", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Sudo et al.", "parsedDate": "2002-12", "numChildren": 0 }, "data": { "key": "5VBADES2", "version": 2, "itemType": "journalArticle", "title": "Inflow and outflow of agricultural chemicals in Lake Biwa", "creators": [ { "creatorType": "author", "firstName": "Miki", "lastName": "Sudo" }, { "creatorType": "author", "firstName": "Takuya", "lastName": "Okubo" }, { "creatorType": "author", "firstName": "Takao", "lastName": "Kunimatsu" }, { "creatorType": "author", "firstName": "Senichi", "lastName": "Ebise" }, { "creatorType": "author", "firstName": "Masahisa", "lastName": "Nakamura" }, { "creatorType": "author", "firstName": "Ryoichi", "lastName": "Kaneki" } ], "abstractNote": "Abstract The annual pesticide inputs and outputs crossing the boundary of Lake Biwa were estimated. The inputs were calculated from continuous observations in four rivers flowing into Akani Bay, and from simultaneous observations in 65 influent rivers. The annual losses of pesticide from the watershed to Lake Biwa were 1.7% for esprocarb, 4.8% for mefenacet, 2.3% for thiobencarb, 3.7% for molinate, 9.4% for simetryn and 13.0% for isoprothiolane. The outputs from the lake were estimated from weekly observations in the Seta River. The loss of pesticides discharged downstream through the Seta River, compared with the amount applied, were estimated to be 0.9% for esprocarb, 3.2% for mefenacet, 0.5% for thiobencarb, 1.3% for molinate, 10.0% for simetryn and 5.7% for isoprothiolane. Pesticide outputs generally decreased to 30–80% of the input amounts, although simetryn was retained in the lake without substantial elimination.", "publicationTitle": "Lakes & Reservoirs: Research & Management", "publisher": "", "place": "", "date": "December 2002", "volume": "7", "issue": "4", "section": "", "partNumber": "", "partTitle": "", "pages": "301-308", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Lakes & Reservoirs: Research & Management", "DOI": "10.1046/j.1440-1770.2002.00195.x", "citationKey": "", "url": "http://www.systems.wsu.edu/scripts/wsuall.pl?url=http://search.ebscohost.com/login.aspx?direct=true&db=a9h&AN=8592045&site=ehost-live", "accessDate": "2015-10-19T18:32:14Z", "PMID": "", "PMCID": "", "ISSN": "13205331", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "EBSCOhost", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "AGRICULTURAL chemicals -- Environmental aspects", "type": 1 }, { "tag": "Lake Biwa", "type": 1 }, { "tag": "Pesticide", "type": 1 }, { "tag": "mass balance", "type": 1 }, { "tag": "paddy field", "type": 1 }, { "tag": "water contamination", "type": 1 }, { "tag": "water pollution", "type": 1 } ], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "2J25DXX9", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/2J25DXX9", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/2J25DXX9", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Popovska and Bonacci", "parsedDate": "2007-02-28", "numChildren": 0 }, "data": { "key": "2J25DXX9", "version": 2, "itemType": "journalArticle", "title": "Basic data on the hydrology of Lakes Ohrid and Prespa", "creators": [ { "creatorType": "author", "firstName": "Cvetanka", "lastName": "Popovska" }, { "creatorType": "author", "firstName": "Ognjen", "lastName": "Bonacci" } ], "abstractNote": "This paper deals with hydrological analyses of Lakes Ohrid and Prespa. The watersheds and the lakes themselves are shared by three countries: Albania, Greece and Macedonia. As a result of insufficient interstate scientific cooperation and inexistence of data exchange, the lakes and their watersheds are not fully investigated regarding hydrology and hydrogeology. This paper represents a first attempt at a complete hydrological analysis based on data from the Macedonian side. This is not considered to be a particular deficiency, because over 60% of the lakes' watersheds and the lakes themselves belong to Macedonia, where a great number of reliable and long-term data series of hydrometeorological observations exist. The Prespa lakes do not have surface outflow and are connected with Lake Ohrid by underground karst conduits. Because of this, from the hydrological point of view, the lakes and their watersheds cannot be analysed separately. The changes of the regime of the air temperature and the rainfall distribution have been investigated in this report. An increase of the maximum and decrease of the minimum annual air temperatures, as well as a decrease of annual precipitation sums has been determined. Also, a statistically significant descending trend of water level in both lakes has been confirmed, with a statement that the water level decrease in Lake Prespa is extremely alarming. From 1985 to 1995 the water level in Lake Prespa has dropped by more than 5 m. The main reasons for this cannot be identified easily because there are no data on water use quantities from all three countries. As the lakes represent unique natural, ecological and economical water resources in a region suffering water shortage, we plead for a strengthening of international support in activities on salvation of both lakes. A prerequisite for this is the water balance calculation and common cooperation in sustainable water resources management of the lakes. Copyright © 2006 John Wiley & Sons, Ltd.", "publicationTitle": "Hydrological Processes", "publisher": "", "place": "", "date": "February 28, 2007", "volume": "21", "issue": "5", "section": "", "partNumber": "", "partTitle": "", "pages": "658-664", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Hydrol. Process.", "DOI": "10.1002/hyp.6252", "citationKey": "", "url": "http://onlinelibrary.wiley.com/doi/10.1002/hyp.6252/abstract", "accessDate": "2015-10-19T18:22:45Z", "PMID": "", "PMCID": "", "ISSN": "1099-1085", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "en", "libraryCatalog": "Wiley Online Library", "callNumber": "", "rights": "Copyright © 2006 John Wiley & Sons, Ltd.", "extra": "", "tags": [ { "tag": "Lake Ohrid", "type": 1 }, { "tag": "Lake Prespa", "type": 1 }, { "tag": "Precipitation", "type": 1 }, { "tag": "karst hydrology", "type": 1 }, { "tag": "water level", "type": 1 } ], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "IBRVXBE3", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/IBRVXBE3", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/IBRVXBE3", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Kadioğlu et al.", "parsedDate": "1997", "numChildren": 0 }, "data": { "key": "IBRVXBE3", "version": 2, "itemType": "journalArticle", "title": "The greatest soda-water lake in the world and how it is influenced by climatic change", "creators": [ { "creatorType": "author", "firstName": "M.", "lastName": "Kadioğlu" }, { "creatorType": "author", "firstName": "Z.", "lastName": "Şen" }, { "creatorType": "author", "firstName": "E.", "lastName": "Batur" } ], "abstractNote": "Global warming resulting from increasing greenhouse gases in the atmosphere and the local climate changes that follow affect local hydrospheric and biospheric environments. These include lakes that serve surrounding populations as a fresh water resource or provide regional navigation. Although there may well be steady water-quality alterations in the lakes with time, many of these are very much climate-change dependent. During cool and wet periods, there may be water-level rises that may cause economic losses to agriculture and human activities along the lake shores. Such rises become nuisances especially in the case of shoreline settlements and low-lying agricultural land. Lake Van, in eastern Turkey currently faces such problems due to water-level rises. The lake is unique for at least two reasons. First, it is a closed basin with no natural or artificial outlet and second, its waters contain high concentrations of soda which prevent the use of its water as a drinking or agricultural water source. Consequently, the water level fluctuations are entirely dependent on the natural variability of the hydrological cycle and any climatic change affects the drainage basin. In the past, the lake-level fluctuations appear to have been rather systematic and unrepresentable by mathematical equations. Herein, monthly polygonal climate diagrams are constructed to show the relation between lake level and some meteorological variables, as indications of significant and possible climatic changes. This procedure is applied to Lake Van, eastern Turkey, and relevant interpretations are presented.", "publicationTitle": "Ann. Geophys.", "publisher": "", "place": "", "date": "1997", "volume": "15", "issue": "11", "section": "", "partNumber": "", "partTitle": "", "pages": "1489-1497", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Ann. Geophys.", "DOI": "10.1007/s00585-997-1489-9", "citationKey": "", "url": "http://www.ann-geophys.net/15/1489/1997/", "accessDate": "2015-10-19T18:07:48Z", "PMID": "", "PMCID": "", "ISSN": "1432-0576", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Copernicus Online Journals", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Lake Van" } ], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "PW3RIRN9", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/PW3RIRN9", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/PW3RIRN9", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Rosagaron", "parsedDate": "2001", "numChildren": 0 }, "data": { "key": "PW3RIRN9", "version": 2, "itemType": "conferencePaper", "title": "Lake Lanao: Its past and present status.", "creators": [ { "creatorType": "author", "firstName": "Roman P.", "lastName": "Rosagaron" } ], "abstractNote": "Geographically located in Central Mindanao, Lake Lanao is the second largest lake in the Philippines. The lake is famous locally for its various uses and internationally for its endemic cyprinids. This paper intends to inform the local leaders and the national planners about Lake Lanao's dwindling fisheries resources, the extinction of some endemic cyprinids, and the current interventions as well as suggested action plans to increase fish production and to conserve the remaining species in the lake. The past and present studies on the lake are also reviewed. Early and latest statistics on the lake's fisheries production are presented to invite the interest of all sectors in coming up with the integrated approach to protect, conserve and increase its fisheries production. Local and national interventions to conserve and increase fisheries production are discussed. These include the setting up of BFAR Fisheries Station in Kialdan, Marantao; the establishment of a fish hatchery in Poona, Marantao by Southern Philippines Development Authority; the formation of Save Lake Lanao Movement by the local leaders; the creation of Lake Lanao Research and Development Council; the current concern of Philippine Council for Aquatic and Marine Research and Development-DOST; and the extension and research and development thrusts of the Mindanao State University, College of Fisheries in Marawi City.", "proceedingsTitle": "", "conferenceName": "", "publisher": "SEAFDEC Aquaculture Department", "place": "", "date": "2001", "eventPlace": "", "volume": "", "issue": "", "numberOfVolumes": "", "pages": "29-39", "series": "", "seriesNumber": "", "DOI": "", "ISBN": "971-8511-53-9", "citationKey": "", "url": "http://repository.seafdec.org.ph/handle/10862/822", "accessDate": "2015-10-19T17:55:06Z", "ISSN": "", "archive": "", "archiveLocation": "", "shortTitle": "Lake Lanao", "language": "en", "libraryCatalog": "repository.seafdec.org.ph", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "M5VZUZ3A", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/M5VZUZ3A", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/M5VZUZ3A", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Avramoski et al.", "numChildren": 0 }, "data": { "key": "M5VZUZ3A", "version": 2, "itemType": "report", "title": "Lake Ohrid Experience and Lessons Learned Brief", "creators": [ { "creatorType": "author", "firstName": "Oliver", "lastName": "Avramoski" }, { "creatorType": "author", "firstName": "Sandri", "lastName": "Kycyku" }, { "creatorType": "author", "firstName": "Trajce", "lastName": "Naumoski" }, { "creatorType": "author", "firstName": "Dejan", "lastName": "Panovski" }, { "creatorType": "author", "firstName": "Veli", "lastName": "Puka" }, { "creatorType": "author", "firstName": "Lirim", "lastName": "Selfo" }, { "creatorType": "author", "firstName": "Mary", "lastName": "Watzin" } ], "abstractNote": "", "reportNumber": "", "reportType": "", "institution": "", "place": "", "date": "", "seriesTitle": "Towards a Lake Basin Management Initiative and a Contribution to the Third World Water Forum: Sharing Experiences and Early Lessons in GEF and non-GEF Lake Basin Management Projects", "seriesNumber": "", "pages": "", "DOI": "", "ISBN": "", "citationKey": "", "url": "http://www.ais.unwater.org/ais/aiscm/getprojectdoc.php?docid=324", "accessDate": "", "ISSN": "", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "", "callNumber": "", "rights": "", "extra": "See also: http://www.ais.unwater.org/ais/aiscm/getprojectdoc.php?docid=324", "tags": [], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "M4F23TMZ", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/M4F23TMZ", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/M4F23TMZ", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Computer Systems Group (CSG)", "parsedDate": "2015-10-15", "numChildren": 0 }, "data": { "key": "M4F23TMZ", "version": 2, "itemType": "webpage", "title": "Report - Documents - IW:Science", "creators": [ { "creatorType": "author", "firstName": "University of Waterloo / The Centre for Community Mapping (COMAP)", "lastName": "Computer Systems Group (CSG)" } ], "abstractNote": "", "websiteTitle": "", "websiteType": "", "date": "2015-10-15", "publisher": "", "place": "", "DOI": "", "citationKey": "", "url": "http://projects.inweh.unu.edu/inweh/report.php?ListType=ProjectDocument&MenuItemID=3&ID=104", "accessDate": "2015-10-15T17:01:40Z", "shortTitle": "Report - Documents - IW", "language": "en", "rights": "", "extra": "", "tags": [], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "RID5WNJ9", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/RID5WNJ9", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/RID5WNJ9", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Turner et al.", "parsedDate": "1996-11-01", "numChildren": 0 }, "data": { "key": "RID5WNJ9", "version": 2, "itemType": "journalArticle", "title": "The geochemistry of Lake Bosumtwi, a hydrologically closed basin in the humid zone of tropical Ghana", "creators": [ { "creatorType": "author", "firstName": "Benjamin F.", "lastName": "Turner" }, { "creatorType": "author", "firstName": "L. R.", "lastName": "Gardner" }, { "creatorType": "author", "firstName": "W E.", "lastName": "Sharp" }, { "creatorType": "author", "firstName": "E. R.", "lastName": "Blood" } ], "abstractNote": "This article is in Free Access Publication and may be downloaded using the “Download Full Text PDF” link at right.", "publicationTitle": "Limnology and Oceanography", "publisher": "", "place": "", "date": "November 1, 1996", "volume": "41", "issue": "7", "section": "", "partNumber": "", "partTitle": "", "pages": "1415-1424", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Limnol. Oceanogr.", "DOI": "10.4319/lo.1996.41.7.1415", "citationKey": "", "url": "http://onlinelibrary.wiley.com/doi/10.4319/lo.1996.41.7.1415/abstract", "accessDate": "2015-10-14T21:53:48Z", "PMID": "", "PMCID": "", "ISSN": "1939-5590", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "en", "libraryCatalog": "Wiley Online Library", "callNumber": "", "rights": "© 1996, by the Association for the Sciences of Limnology and Oceanography, Inc.", "extra": "", "tags": [], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "8WA4CBMP", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/8WA4CBMP", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/8WA4CBMP", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Desiage et al.", "parsedDate": "2015-11-01", "numChildren": 0 }, "data": { "key": "8WA4CBMP", "version": 2, "itemType": "journalArticle", "title": "Deglacial and postglacial evolution of the Pingualuit Crater Lake basin, northern Québec (Canada)", "creators": [ { "creatorType": "author", "firstName": "Pierre-Arnaud", "lastName": "Desiage" }, { "creatorType": "author", "firstName": "Patrick", "lastName": "Lajeunesse" }, { "creatorType": "author", "firstName": "Guillaume", "lastName": "St-Onge" }, { "creatorType": "author", "firstName": "Alexandre", "lastName": "Normandeau" }, { "creatorType": "author", "firstName": "Grégoire", "lastName": "Ledoux" }, { "creatorType": "author", "firstName": "Hervé", "lastName": "Guyard" }, { "creatorType": "author", "firstName": "Reinhard", "lastName": "Pienitz" } ], "abstractNote": "The Pingualuit Crater, located in the Ungava Peninsula (northern Québec, Canada) is a 1.4-Ma-old impact crater hosting a ~ 245-m-deep lake. The lake has a great potential to preserve unique paleoclimatic and paleoecological sedimentary records of the last glacial/interglacial cycles in the terrestrial Canadian Arctic. In order to investigate the stratigraphy in the lake and the late Quaternary glacial history of the Pingualuit Crater, this study compiles data from three expeditions carried out in May 2007 (~ 9-m-long sediment core), in August 2010 (~ 50 km of seismic lines), and in September 2012 (high-resolution terrestrial LiDAR topography of the inner slopes). Despite the weak penetration (~ 10 m) of the 3.5-kHz subbottom profiling caused by the presence of boulders in the sedimentary column, seismic data coupled with the stratigraphy established from the sediment core enabled the identification of two glaciolacustrine units deposited during the final stages of the Laurentide Ice Sheet (LIS) retreat in the crater. Two episodes of postglacial mass wasting events were also identified on the slopes and in the deep basin of the crater. The high-resolution topography of the internal slopes of the crater generated from the LiDAR data permitted the confirmation of a paleolake level at 545 m and determination of the elevation of drainage outlets. Together with the mapping of glacial and deglacial landforms from air photographs, the LiDAR data allowed the development of a new deglaciation and drainage scenario for the Pingualuit Crater Lake and surrounding area. The model proposes three main phases of lake drainage, based on the activation of seven outlets following the retreat of the LIS front toward the southwest. Finally, as opposed to other high-latitude crater lake basins such as Lake El'gygytgyn or Laguna Potrok Aike where high-resolution paleoclimatic records were obtained owing to high sediment accumulation rates, the seismic data from the Pingualuit Crater Lake suggest extremely low sedimentation rates after the retreat of the LIS owing to the absence of tributaries.", "publicationTitle": "Geomorphology", "publisher": "", "place": "", "date": "November 1, 2015", "volume": "248", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "327-343", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Geomorphology", "DOI": "10.1016/j.geomorph.2015.07.023", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S0169555X15300866", "accessDate": "2015-10-14T21:48:25Z", "PMID": "", "PMCID": "", "ISSN": "0169-555X", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Arctic", "type": 1 }, { "tag": "Laurentide Ice Sheet", "type": 1 }, { "tag": "LiDAR", "type": 1 }, { "tag": "Mass movements", "type": 1 }, { "tag": "Sedimentological processes", "type": 1 }, { "tag": "lake levels", "type": 1 } ], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "TSZDDIAD", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/TSZDDIAD", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/TSZDDIAD", "type": "text/html" } }, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Guyard et al.", "parsedDate": "2011-12", "numChildren": 0 }, "data": { "key": "TSZDDIAD", "version": 2, "itemType": "journalArticle", "title": "New insights into Late Pleistocene glacial and postglacial history of northernmost Ungava (Canada) from Pingualuit Crater Lake sediments", "creators": [ { "creatorType": "author", "firstName": "Hervé", "lastName": "Guyard" }, { "creatorType": "author", "firstName": "Guillaume", "lastName": "St-Onge" }, { "creatorType": "author", "firstName": "Reinhard", "lastName": "Pienitz" }, { "creatorType": "author", "firstName": "Pierre", "lastName": "Francus" }, { "creatorType": "author", "firstName": "Bernd", "lastName": "Zolitschka" }, { "creatorType": "author", "firstName": "Garry K. C.", "lastName": "Clarke" }, { "creatorType": "author", "firstName": "Sonja", "lastName": "Hausmann" }, { "creatorType": "author", "firstName": "Veli-Pekka", "lastName": "Salonen" }, { "creatorType": "author", "firstName": "Patrick", "lastName": "Lajeunesse" }, { "creatorType": "author", "firstName": "Grégoire", "lastName": "Ledoux" }, { "creatorType": "author", "firstName": "Michel", "lastName": "Lamothe" } ], "abstractNote": "The Pingualuit Crater was formed by a meteoritic impact ca. 1.4 million years ago in northernmost Ungava (Canada). Due to its geographical position near the center of successive North American ice sheets and its favorable morphometry, the Pingualuit Crater Lake (water depth = 246 m) promises to yield a unique continuous sedimentary sequence covering several glacial/interglacial cycles in the terrestrial Canadian Arctic. In this paper, we suggest the existence of a subglacial lake at least during the Last Glacial Maximum (LGM) by hydraulic potential modeling using LGM ice-surface elevation and bed topography derived from a digital elevation model. These results support the hypothesis that the bottom sediments of the Crater Lake escaped glacial erosion and may contain a long-term continental sedimentary sequence. We also present the stratigraphy of a 9 m-long core retrieved from the deep basin of the lake as well as a multiproxy reconstruction of its deglacial and postglacial history. The base of the core is formed by very dense diamicton reflecting basal melt-out environments marking the end of subglacial conditions at the coring site. The overlying finely laminated silt are related to the onset of proglacial conditions characterized by extremely low lacustrine productivity. Infra Red Stimulated Luminescence and AMS 14C dating, as well as biostratigraphic data indicate sediment mixing between recent (e.g. Holocene) and much older (pre- to mid-Wisconsinan) material reworked by glacier activity. This process prevents the precise dating of these sediments that we interpret as being deposited just before the final deglaciation of the lake. Two finer grained and organic-rich intervals reflect the inception of lacustrine productivity resulting from the cessation of glacial meltwater inputs and ice-free periods. The lower organic interval corresponds to the early postglacial period (6850–5750 cal BP) and marks the transition between proglacial and postglacial conditions during the Holocene Thermal Maximum, while the uppermost organic-rich core section represents late Holocene sediments (∼4200–600 cal BP). The organic intervals are separated by a basin-scale erosive slide occurring around 4200 cal BP and likely related to 1) a seismic event due to the glacio-isostatic rebound following the last deglaciation or 2) slope instabilities associated with rapid discharge events of the lake.", "publicationTitle": "Quaternary Science Reviews", "publisher": "", "place": "", "date": "December 2011", "volume": "30", "issue": "27–28", "section": "", "partNumber": "", "partTitle": "", "pages": "3892-3907", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Quaternary Science Reviews", "DOI": "10.1016/j.quascirev.2011.10.002", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S0277379111003064", "accessDate": "2015-10-14T21:47:53Z", "PMID": "", "PMCID": "", "ISSN": "0277-3791", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Crater Lake", "type": 1 }, { "tag": "Lacustrine sediments", "type": 1 }, { "tag": "Late Pleistocene", "type": 1 }, { "tag": "Multiproxy", "type": 1 }, { "tag": "Stratigraphy", "type": 1 }, { "tag": "Subglacial Lake", "type": 1 }, { "tag": "Ungava", "type": 1 } ], "collections": [], "relations": {}, "dateAdded": "2015-10-23T18:06:55Z", "dateModified": "2015-10-23T18:06:55Z" } }, { "key": "TW5KT7N8", "version": 2, "library": { "type": "group", "id": 420663, "name": "Ancient Lakes Hydrology", "links": { "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/420663/items/TW5KT7N8", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/ancient_lakes_hydrology/items/TW5KT7N8", "type": "text/html" }, "up": { "href": "https://api.zotero.org/groups/420663/items/8G9GPABA", "type": "application/json" } }, "meta": { "createdByUser": { "id": 789246, "username": 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}, "meta": { "createdByUser": { "id": 789246, "username": "stephlabou", "name": "", "links": { "alternate": { "href": "https://www.zotero.org/stephlabou", "type": "text/html" } } }, "creatorSummary": "Ackerman", "numChildren": 0 }, "data": { "key": "DCX52A8D", "version": 2, "itemType": "webpage", "title": "Israel Renews Sea of Galilee Flow to Jordan River After 49 Years", "creators": [ { "creatorType": "author", "firstName": "Gwen", "lastName": "Ackerman" } ], "abstractNote": "For the first time since 1964, Israel will allow Sea of Galilee water to flow into the Jordan River as part of a rehabilitation project that will cost millions of shekels, the Israel Water Authority said.", "websiteTitle": "Bloomberg.com", "websiteType": "", "date": "", "publisher": "", "place": "", "DOI": "", "citationKey": "", "url": "http://www.bloomberg.com/news/articles/2013-05-26/israel-renews-sea-of-galilee-flow-to-jordan-river-after-49-years", "accessDate": "2015-10-23T17:05:33Z", "shortTitle": "", 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