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            "title": "Microbial Ecology of Rotten Sea Ice: Implications for Arctic Carbon Cycling with Global Warming",
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                    "creatorType": "author",
                    "firstName": "Carie M.",
                    "lastName": "Frantz"
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                    "creatorType": "author",
                    "firstName": "Byron C.",
                    "lastName": "Crump"
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                    "firstName": "Mónica V.",
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            "abstractNote": "“Rotten” sea ice, ice in an advanced stage of melt, represents an important but understudied habitat in the rapidly changing Arctic. As Arctic warming accelerates, this late-season ice type will become more prevalent, yet little is known about its microbial inhabitants or their roles in Arctic marine biogeochemical cycles. We examined microbial communities (prokaryote and algal abundance, 16S and 18S rRNA gene and transcript sequencing) and biogeochemical properties of rotten sea ice and earlier-season ice near Utqiaġvik, Alaska, USA. Rotten ice was comparatively warm, isothermal, and largely drained of brine, with extensive, interconnected pore networks linked to melt ponds above and seawater below. Unlike earlier-season ice, fluids saturating rotten ice were vertically homogeneous in pH, dissolved inorganic carbon, prokaryote and phytoplankton abundance, and microbial community composition. However, particulate carbon and nitrogen exhibited strong vertical gradients, with the highest concentrations near the surface. Microbial communities in rotten ice were significantly different from those in earlier-season ice and varied between individual floes. These findings indicate that rotten ice constitutes a distinct microbial habitat and may serve as an important source of nutrient-rich particulate matter in the future Arctic Ocean during the summer melt season.",
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            "title": "Patterns of trophic niche overlap of diadromous and marine Arctic fishes in Beaufort Sea coastal lagoons",
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                    "firstName": "Sydney",
                    "lastName": "Wilkinson"
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                    "firstName": "Lara",
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                    "creatorType": "author",
                    "firstName": "Benjamin D.",
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            "abstractNote": "Ongoing climatic changes in the coastal Arctic can influence the food webs that support a variety of fish species and subsistence fisheries in coastal lagoons. Along the Beaufort Sea coast, lagoons provide productive summer feeding habitats for both diadromous fishes migrating from freshwater and marine fishes migrating from the shelf. We compared trophic niche size and niche overlap between diadromous species, Arctic Cisco (Coregonus autumnalis), Least Cisco (Coregonus sardinella), and Dolly Varden (Salvelinus malma), and marine species, Polar Cod (Boreogadus saida), Fourhorn Sculpin (Myoxocephalus quadricornis), and Saffron Cod (Eleginus gracilis), across lagoon systems differing in freshwater input and oceanic exchange. Using complementary biomarkers (stomach contents, bulk δ13C and δ15N, compound-specific amino acid δ13C, and fatty acid profiles), we found that diadromous fishes consistently exhibited broader trophic niches than marine fishes, reflecting their ability to exploit both freshwater and offshore pelagic resources. Trophic overlap occurred across the two life histories in both lagoon types, but was greater in high-exchange lagoons, primarily due to shared reliance on amphipods, mysids, and marine carbon sources. Considering the different biomarker turnover times, this overlap likely extends from late winter ice cover into open water periods. These results suggest that competition for prey is probable among species with contrasting life histories, particularly during periods of low prey abundance. By resolving seasonal and spatial patterns of trophic overlap, our findings provide important baseline knowledge for modeling future scenarios of lagoon connectivity and for informing subsistence fisheries management under ongoing changes in the Arctic.",
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            "title": "Hydrological and Thermal Dynamics of a Supra-Permafrost Subterranean Estuary",
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                    "firstName": "Cansu",
                    "lastName": "Demir"
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                    "firstName": "Emma",
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                    "firstName": "Matthew A.",
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                    "firstName": "M. Bayani",
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            "abstractNote": "Subterranean estuaries (STEs), where groundwater interacts with seawater, influence surface and subsurface coastal ecology and biogeochemistry. In Arctic-STEs overlying permafrost, groundwater flow and heat transport determine the fate of organic matter. Yet, direct observations of groundwater flow and heat and solute transport processes in Arctic STEs remain limited. This study characterized groundwater flow paths and fluxes and heat transport within an Arctic-STE along Alaska's Beaufort Sea coast during thawing, summer, and freeze-up. Intertidal seabed temperature-depth profiles collected along a 10-m transect captured the active groundwater flow period, from thaw and flow onset in mid-June to freeze-up in late-September. During this period, aquifer geometry evolved non-uniformly due to spatially varying thaw rates across the STE (mean (m) thaw depths–beach: 0.25 to 0.55–0.6 m on 20 June, 25 July, 1 October; seabed: 0.6–0.9 m from 25 July to 1 October). Groundwater and surface water levels, salinity, and subsurface temperature profiles measured over tidal time scales were interpreted alongside groundwater flow-heat transport numerical simulations. Fresh groundwater discharge was sporadic during thawing (m: 0.32 m3/day/m), abundant in summer (m: 0.45 m3/day/m), and was largely absent during freeze-up. During freeze-up, groundwater flow was driven exclusively by seawater recirculation via tidal pumping (from thawing to summer to freeze-up: 0.00025–0.15–0.5 m3/day/m) and convection. Heat advection dominated near aquatic interfaces (shaping intertidal ice), and conduction controlled vertical temperature gradients in low-flow and unsaturated sediments. These findings will help predict how prolonged summers will alter Arctic-STE cryo-hydrology and biogeochemistry.",
            "publicationTitle": "Water Resources Research",
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            "date": "2026",
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            "title": "Elucidating the Reactivity and Fate of Dissolved Organic Matter in Groundwater Entering the Alaska Beaufort Sea Coast Using <sup>14</sup>C Ramped Oxidation",
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                    "creatorType": "author",
                    "firstName": "C. T.",
                    "lastName": "Connolly"
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                    "firstName": "R. G. M.",
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                    "firstName": "J. W.",
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            "abstractNote": "Ramped oxidation and isotopic analysis provide a framework for assessing organic matter transformation and fate across Arctic waters\n\nSupra-permafrost groundwater exhibits an aged but reactive mid...",
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    {
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            "title": "The Evolving Decline of Landfast Sea Ice in Northern Alaska and Adjacent Waters: Results from an Updated Climatology",
            "creators": [
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                    "creatorType": "author",
                    "firstName": "Andrew R.",
                    "lastName": "Mahoney"
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                    "creatorType": "author",
                    "firstName": "Andrew H.",
                    "lastName": "Einhorn"
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            "abstractNote": "We present a new 27-year record of landfast sea ice extent in northern Alaska and adjacent waters, which uses ice chart data to extend a previous analysis based on synthetic aperture radar (SAR) imagery. This new climatology provides updated information on the decline of landfast ice in a region of the Arctic that has seen extensive losses of sea ice in recent summers. By comparing our results with early satellite data analysis from the 1970s, we find that trends in the timing of landfast ice have been ongoing for at least 50 years. Over the period 1996–2023, the landfast season shortened by 19 days/decade in the Chukchi Sea and 13 days/decade in the Beaufort Sea, primarily due to later formation of landfast ice. Also, the time between onset of freezing air temperatures and landfast ice formation is increasing, which is consistent with a coastal ocean that takes longer to freeze. While it was previously reported that the typical annual maximum width of landfast ice in the Chukchi Sea declined by 13 km between periods 1970–1976 and 1996–2008, we find this retreat has slowed with a decline of 3.3 km over the course of our data set as few areas of extensive landfast remain to be lost. Conversely, landfast sea ice extent in the Beaufort Sea had previously been found to have remained constant since the 1970s, but we find an average reduction of 2.5 km. We attribute this emergent phenomenon to a reduction in the number grounded ridges forming offshore.",
            "publicationTitle": "Journal of Geophysical Research: Oceans",
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            "date": "2026",
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            "PMCID": "",
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            "shortTitle": "The Evolving Decline of Landfast Sea Ice in Northern Alaska and Adjacent Waters",
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                    "firstName": "Alina C.",
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            "abstractNote": "Coastal flooding and saltwater intrusion (SWI) pose growing threats to Arctic coastal permafrost, yet their long-term impacts remain poorly understood. While prior studies focused on surface effects like vegetation dieback or lake salinization, subsurface hydrothermal observations in salinized coastal tundra are lacking. This study investigates both surface and subsurface effects of SWI on tundra and active layer thermal regimes in an area with previously recorded impacts from recurring seawater inundation. Seawater flooding in the study area was driven by western winds; flooding intensity and frequency varied along an elevation gradient, influencing vegetation cover and porewater salinity. Low-lying, frequently inundated areas had sparse vegetation and mineral sediment deposition, while higher elevation areas remained non-salinized with high vegetation cover, as indicated by NDVI. Frequently flooded sites had deeper thaw depths, and temperature profiles revealed these areas experienced summer soil temperatures up to 12 °C warmer than non-inundated sites. We attribute increased ground heat flux to a combination of a lack of vegetation, which reduces ground insulation and shading, and increased thermal diffusivity from mineral sediment deposition during inundation. These findings uncover an overlooked feedback loop between elevation, salinization, and tundra active layer thermal regime. Inundation frequency and coastal land loss will likely increase in response to changing climate. This study highlights SWI as an emerging threat to coastal Arctic resilience by revealing its coupled surface and subsurface thermal impacts.",
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                    "creatorType": "author",
                    "firstName": "Emily M.",
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                    "firstName": "Megan I.",
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            "abstractNote": "Supra-permafrost groundwater (SPGW) flowing through seasonally thawed soils is an important source of dissolved organic matter (DOM) to the Arctic Ocean, yet few studies have investigated the quality of this DOM. We sampled SPGW, runoff, and rivers near Simpson Lagoon, Alaska, during spring ice breakup, summer open water, and fall freeze-up seasons. Through incubation experiments, we compared biodegradable DOC (BDOC) across sources and seasons and linked these results with DOM composition using Fourier-transform ion cyclotron resonance mass spectrometry (FT-ICR MS). DOM composition was distinctly different between SPGW and rivers and shifted throughout the year. SPGW contained an order of magnitude more dissolved organic carbon (DOC) than rivers, with average concentrations increasing from breakup (22 ± 5 mg C L–1) to freeze-up (110 ± 42 mg C L–1). SPGW also contained three times or more BDOC than rivers, averaging 18 ± 1% during breakup and declining to 3.4 ± 0.7% during freeze-up. BDOC was positively correlated with condensed aromatic and polyphenolic DOM formula classes that are often associated with recalcitrant organic matter. Thus, SPGW DOM is highly aromatic yet biodegradable and is likely an important energy source to Arctic coastal waters in summer when river inputs are low.",
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            "title": "Trophic niche variation across the pan-Arctic coastal continuum",
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                    "creatorType": "author",
                    "firstName": "Nathan D.",
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                    "firstName": "Guillaume",
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                    "creatorType": "author",
                    "firstName": "Rolf",
                    "lastName": "Gradinger"
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                {
                    "creatorType": "author",
                    "firstName": "Joanna",
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                    "firstName": "Maeve",
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                    "firstName": "Frédéric",
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                    "firstName": "Paul E.",
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                    "firstName": "Janne E.",
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                    "firstName": "Maria",
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                    "firstName": "Kenneth H.",
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            "abstractNote": "We analyzed stable carbon and nitrogen isotope values (δ13C and δ15N, respectively) for pan-Arctic coastal primary producers and consumers to detect large-scale regional trends both temporally and spatially. To facilitate comparison, we grouped coastal habitats into fjords, lagoons, shelves, and straits as four “coastscapes”. We gathered over 12,000 rows of data collected over 24 years (between 1999 and 2022) from 34 different field campaigns across the coastal Arctic (63 to 81°N and 177°W to 33°E). Our goal was to examine the isotopic patterns in pelagic and sediment particulate organic matter (pPOM and sPOM, respectively) and four consumer groups (deposit feeders, opportunists/scavengers, predators, and suspension feeders) among the four coastscapes. We found that despite the enormous spatial range of data, both pPOM and sPOM became 2.1‰ and 2.2‰ more 13C-depleted per decade, respectively, with parallel decreases in the δ13C values in consumers. The significant decrease is likely attributed to the increased contributions of 13C-depleted terrestrial organic matter across the Arctic coasts from freshwater inputs and coastal erosion in concert with diminishing sea ice that supports sympagic microalgae. Across all Arctic coastscapes, consumer groups exhibited overlapping isotopic composition, notably with wide δ13C ranges that indicated assimilation of multiple organic matter sources, including terrestrial organic matter, organic matter derived from marine phytoplankton and sea ice algae, macroalgae, and potentially benthic microalgae or degraded organic matter. This consistent pattern across coastscapes provides evidence of the trophic plasticity possessed by Arctic consumers, how coastal food webs respond to climate warming, and the signature of terrestrialization imprinted on the pan-Arctic coastal isoscape.",
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            "abstractNote": "Arctic cod (Boreogadus saida, also called polar cod) are considered the single most important Arctic forage fish due to their high abundance and nutritional quality. Because Arctic cod are strongly ice associated and prefer colder waters, their frequency in coastal waters has declined with warming, decreasing availability to nearshore predators. To consider the nutritional quality of alternative prey, we measured energy density and estimated whole-body energy of forage-size (39–200 mm) fishes collected during summers 2021–2023 (n = 274). The fishes sampled included 16 potential prey species from Foggy Island Bay (70.3°N, 147.5°W, near Prudhoe Bay) and Lion Bay (70.2°N, 146.4°W, near Flaxman Island), northern Alaska. Dry weight energy densities ranged from 16.2 to 27.5 kJ g-1 (mean ± SD = 22.0 ± 1.73 kJ g-1, n = 274) across individuals. Of common species, Arctic cod had the highest mean energy density (24.3 ± 1.1 kJ g-1, n = 25) and fourhorn sculpin (Myoxocephalus quadricornis) had the lowest (19.7 ± 0.8 kJ g-1, n = 20). To account for size differences among prey species, whole-body energy of typical fish sizes available to predators were modeled using whole-body energy to length relationships and length distributions. Juvenile salmonids (e.g., ciscoes and whitefishes) provided the most energy per individual and were four-fold greater than smaller-bodied Arctic cod. Predators that consume juvenile ciscoes and whitefishes may be more resilient to declines in Arctic cod availability than predators with smaller gapes.",
            "publicationTitle": "Marine Biology",
            "publisher": "",
            "place": "",
            "date": "2025-09-17",
            "volume": "172",
            "issue": "10",
            "section": "",
            "partNumber": "",
            "partTitle": "",
            "pages": "157",
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            "seriesTitle": "",
            "seriesText": "",
            "journalAbbreviation": "Mar Biol",
            "DOI": "10.1007/s00227-025-04705-5",
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            "url": "https://doi.org/10.1007/s00227-025-04705-5",
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            "language": "en",
            "libraryCatalog": "Springer Link",
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            "extra": "https://doi.org/10.5066/P13ELTUB",
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                    "tag": "Arctic",
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                },
                {
                    "tag": "Energy content",
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                },
                {
                    "tag": "Energy density",
                    "type": 1
                },
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                },
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        "key": "3L68G6CL",
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            "title": "Quantitative metatranscriptomics and biogeochemical rate measurements reveal microbial pathways driving carbon and nitrogen cycles in an Arctic coastal lagoon",
            "creators": [
                {
                    "creatorType": "author",
                    "firstName": "Natasha A.",
                    "lastName": "Griffin"
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                {
                    "creatorType": "author",
                    "firstName": "Brian",
                    "lastName": "Kim"
                },
                {
                    "creatorType": "author",
                    "firstName": "Amber K.",
                    "lastName": "Hardison"
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                {
                    "creatorType": "author",
                    "firstName": "Byron C.",
                    "lastName": "Crump"
                }
            ],
            "abstractNote": "Microbial communities in Arctic coastal lagoons mediate nitrogen and carbon cycling at the terrestrial–marine interface of these rapidly changing ecosystems. To investigate these microbial processes, we measured gene expression, nitrification, and inorganic carbon assimilation in waters of Elson Lagoon on the Beaufort Sea coast under ice cover (April), during spring break-up (July), and in open water (August). Quantitative metatranscriptomics with internal controls quantified per-liter transcript abundances alongside in situ light and dark 15N-ammonium, 15N-urea, and 13C-bicarbonate stable isotope tracer incubations. Nitrification was only detectable during ice cover, showing high rates for Arctic coastal systems and evidence of light inhibition. Although carbon assimilation was relatively low during ice cover, dark carbon assimilation accounted for nearly half of total uptake, matching estimates of chemoautotrophic potential based on nitrification. Microbial gene expression also shifted seasonally in abundance and function. Transcripts for nitrification peaked during ice cover when genes for ammonia oxidation and 3-HP/4-HB carbon fixation were primarily expressed by archaeal genus Nitrosopumilus, while those for nitrite oxidation and reverse TCA carbon fixation were expressed by bacterial phylum Nitrospinota. During break-up and open water, expression shifted toward urea metabolism, nitrogen assimilation, Calvin Cycle carbon fixation, and anaplerotic pathways. These shifts highlight the seasonality of microbial metabolic strategies and reveal distinct functional shifts across the Arctic lagoon seasonal cycle. The findings suggest that ongoing warming and declining ice cover may reduce chemoautotrophic activity and alter nitrogen and carbon cycling under future conditions, with implications for nutrient dynamics and primary production in Arctic coastal ecosystems.",
            "publicationTitle": "Limnology and Oceanography",
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            "DOI": "10.1002/lno.70257",
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            "title": "Deep learning estimation of northern hemisphere soil freeze-thaw dynamics using satellite multi-frequency microwave brightness temperature observations",
            "creators": [
                {
                    "creatorType": "author",
                    "firstName": "Kellen",
                    "lastName": "Donahue"
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                    "creatorType": "author",
                    "firstName": "John S.",
                    "lastName": "Kimball"
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                    "firstName": "Jinyang",
                    "lastName": "Du"
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                    "firstName": "Andreas",
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                    "firstName": "Mahta",
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                    "firstName": "Jesse",
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                    "firstName": "Youngwook",
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                {
                    "creatorType": "author",
                    "firstName": "Michael A.",
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            "abstractNote": "Satellite microwave sensors are well suited for monitoring landscape freeze-thaw (FT) transitions owing to the strong brightness temperature (TB) or backscatter response to changes in liquid water abundance between predominantly frozen and thawed conditions. The FT retrieval is also a sensitive climate indicator with strong biophysical importance. However, retrieval algorithms can have difficulty distinguishing the FT status of soils from that of overlying features such as snow and vegetation, while variable land conditions can also degrade performance. Here, we applied a deep learning model using a multilayer convolutional neural network driven by AMSR2 and SMAP TB records, and trained on surface (~0–5 cm depth) soil temperature FT observations. Soil FT states were classified for the local morning (6 a.m.) and evening (6 p.m.) conditions corresponding to SMAP descending and ascending orbital overpasses, mapped to a 9 km polar grid spanning a five-year (2016–2020) record and Northern Hemisphere domain. Continuous variable estimates of the probability of frozen or thawed conditions were derived using a model cost function optimized against FT observational training data. Model results derived using combined multi-frequency (1.4, 18.7, 36.5 GHz) TBs produced the highest soil FT accuracy over other models derived using only single sensor or single frequency TB inputs. Moreover, SMAP L-band (1.4 GHz) TBs provided enhanced soil FT information and performance gain over model results derived using only AMSR2 TB inputs. The resulting soil FT classification showed favorable and consistent performance against soil FT observations from ERA5 reanalysis (mean percent accuracy, MPA: 92.7%) and in situ weather stations (MPA: 91.0%). The soil FT accuracy was generally consistent between morning and afternoon predictions and across different land covers and seasons. The model also showed better FT accuracy than ERA5 against regional weather station measurements (91.0% vs. 86.1% MPA). However, model confidence was lower in complex terrain where FT spatial heterogeneity was likely beneath the effective model grain size. Our results provide a high level of precision in mapping soil FT dynamics to improve understanding of complex seasonal transitions and their influence on ecological processes and climate feedbacks, with the potential to inform Earth system model predictions.",
            "publicationTitle": "Frontiers in Big Data",
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            "date": "2023-11-17",
            "volume": "6",
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            "journalAbbreviation": "Front. Big Data",
            "DOI": "10.3389/fdata.2023.1243559",
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                    "tag": "Microwave",
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                    "tag": "SMAP",
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                },
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                    "tag": "Supported"
                },
                {
                    "tag": "machine learning",
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                {
                    "tag": "soil freeze-thaw",
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                }
            ],
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            "dateAdded": "2025-09-26T20:43:49Z",
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            "title": "Local environmental conditions structured discrete fish assemblages in Arctic lagoons",
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                    "creatorType": "author",
                    "firstName": "Sarah M.",
                    "lastName": "Laske"
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                    "lastName": "von Biela"
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                    "firstName": "Kenneth H.",
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            "abstractNote": "Rapid changes in sea ice extent and changes in freshwater inputs from land are rapidly changing the nature of Arctic estuarine ecosystems. In the Beaufort Sea, these nearshore habitats are known for their high productivity and mix of marine resident and diadromous fishes that have great subsistence value for Indigenous communities. There is, however, a lack of information on the spatial variation among Arctic nearshore fish communities as related to environmental drivers. In summers of 2017–2019, we sampled fishes in four estuarine ecosystems to assess community composition and relate fish abundance to temperature, salinity, and wind conditions. We found fish communities were heterogeneous over larger spatial extents with rivers forming fresh estuarine plumes that supported diadromous species (e.g., broad whitefish Coregonus nasus), while lagoons with reduced freshwater input and higher salinities were associated with marine species (e.g., saffron cod Eleginus gracilis). West–East directional winds accounted for up to 66% of the community variation, indicating importance of the wind-driven balance between fresh and marine water masses. Salinity and temperature accounted for up to 54% and 37% of the variation among lagoon communities, respectively. Recent sea ice declines provide more opportunity for wind to influence oceanographic conditions and biological communities. Current subsistence practices, future commercial fishing opportunities, and on-going oil and gas activities benefit from a better understanding of current fish community distributions. This work provides important data on fish spatial distributions and community composition, providing a basis for fish community response to changing climatic conditions and anthropogenic use.",
            "publicationTitle": "Polar Biology",
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            "pages": "551-568",
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            "title": "Increasing freshwater and dissolved organic carbon flows to Northwest Alaska's Elson lagoon",
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                    "firstName": "Michael A.",
                    "lastName": "Rawlins"
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            "publicationTitle": "Environmental Research Letters",
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            "date": "2021-10",
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