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  • 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous
  • Arctic Ocean
  • American Geophysical Union  (46)
  • MDPI - Multidisciplinary Digital Publishing Institute  (5)
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  • 1
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    MDPI - Multidisciplinary Digital Publishing Institute
    Publication Date: 2024-03-28
    Description: Earth observation (EO), remote sensing (RS), and geoinformation (GI) technologies play a critical role in the study of Svalbard's environment, providing insights into the region's changes and supporting decision-making processes. This reprint presents a comprehensive overview of the applications of EO and RS technologies in Svalbard, covering a wide range of topics related to the environment. It includes contributions from leading experts in the field, providing insights into the current state of the art and future directions for research. The reprint starts by introducing the status of EO and RS in Svalbard, providing a solid foundation for readers new to the field. It then delves into specific applications of these technologies, including the monitoring of glaciers, snow cover, and permafrost using ground-, space-, and air-based RS platforms. Overall, this book aims to provide a comprehensive overview of the applications of EO and RS technologies in Svalbard, highlighting their importance in understanding and addressing the challenges faced by the region. It will be a valuable resource for researchers, students, policymakers, and practitioners in the fields of environmental science, geography, and remote sensing.
    Keywords: snow cover ; remote sensing ; sea ice variability ; vegetation growth ; arctic climate change ; Arctic aerosol ; aerosol transport ; aged aerosol ; aerosol modification ; aerosol optical properties ; aerosol microphysical properties ; aerosol remote sensing ; microphysical inversion ; aerosol radiative effect ; Arctic radiative budget ; earth observation ; COVID-19 ; Svalbard ; earth system science ; SIOS ; polar regions ; snow modelling ; MODIS ; Sentinel-2 ; permafrost ; active layer ; InSAR ; time series ; ground displacement ; ground temperature ; displacement progression ; thaw progression ; Arctic ; NDVI ; time-series ; onset of growth ; classifier ; disturbance ; drone ; ecological monitoring ; GLCM ; herbivore ; random forest ; winter climate effect ; grubbing ; Arctic clouds ; cirrus clouds ; ice clouds ; lidar ; ocean eddies ; marginal ice zone ; sea ice ; SAR imaging ; Fram Strait ; Greenland Sea ; Hopen Island ; Arctic Ocean ; tidewater glaciers ; surface elevation changes ; glacier geometry ; structure-from-motion ; terrestrial laser scanning ; digital elevation model ; ICESat-2 ; laser altimetry ; kinematic GPS experiments ; glaciology ; surge glaciers ; svalbard ; density dimension algorithm for ice surfaces ; airborne validation of satellite data ; lake ice ; Sentinel-1 ; water temperature ; glacier facies ; atmospheric correction ; pansharpening ; WorldView-2 ; Ny-Ålesund ; Chandra–Bhaga basin ; target detection ; supervised classification ; Sentinel-1 and Sentinel-2 ; time series analysis ; snow melt ; tundra ; plant phenology ; ice cover ; Antarctic ; spectral reflectance ; hyperspectral data ; ocean colour ; coastal darkening ; SPM ; sediment plumes ; Arctic coast ; regional tuning ; coastal ecosystems ; land-ocean-interaction ; riverine inputs ; geographic object-based image analysis ; glacier surface facies ; surface facies of glaciers ; pixel-based image analysis ; atmospheric corrections ; image processing routines ; n/a ; thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general ; thema EDItEUR::R Earth Sciences, Geography, Environment, Planning::RG Geography
    Language: English
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  • 2
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    MDPI - Multidisciplinary Digital Publishing Institute
    Publication Date: 2024-03-27
    Description: Around 10% of the global population lives in the world’s coastal zones, mostly concentrated in the world’s largest megacities. In many regions, the population is exposed to a variety of natural hazards and space-based observations. This Special Issue will focus on the usage of remote sensing alone or in synergy with in situ measurments and modeling tools to provide precise and systematic information about processes acting in the world’s coastal zones.
    Keywords: ACOLITE ; coastal waters ; atmospheric correction ; time-series ; management ; Sentinel-2 ; radon transform ; remote sensing ; bathymetry inversion ; multi-scale monitoring ; image augmentation ; phytoplankton remote sensing ; coastal ocean ; red tides ; black pixel assumption ; satellite ; sediment transport ; coastal geomorphology ; ocean color ; GOCI ; VIIRS ; turbid waters ; satellite-derived bathymetry ; Copernicus programme ; multi-temporal approach ; lidar ; turbidity ; coastal upwelling ; wind forcing ; river plume ; MODIS ; Arctic Ocean ; hurricanes ; water quality ; Puerto Rico ; harmful algal blooms ; Chattonella spp. ; Skeletonema spp. ; backscattering ; Ariake Sea ; chlorophyll-a variability ; spring–neap tides ; MODIS-Aqua ; total suspended sediment ; river discharge ; band registration ; morphological registration ; multispectral camera ; Micasense Rededge-M ; Pearl River estuary ; diffuse attenuation coefficient ; S-EOF ; land subsidence ; multi-temporal SAR interferometry ; sea-surface height ; relative sea level change ; satellite altimetry data ; GNSS ; coastal urban centers ; natural protected areas ; climate change impact ; physics-based inversion method ; ocean surface circulation ; high frequency radar ; self-organizing map ; empirical orthogonal function ; neural networks ; synoptic characteristics ; wave radar ; sea waves ; model data ; Mediterranean sea ; small river plume ; aerial drone ; coastal processes ; frontal zones ; internal waves ; along-track interferometric synthetic aperture radar (ATI-SAR) ; current line-of-sight (LOS) velocity ; azimuth ambiguity ; baseline-to-platform speed ratio estimation ; storm surge ; coastal flooding ; marine storms ; natural hazards ; steric-effect ; satellite altimetry ; ADG/CDOM colored dissolved organic matter ; Sentinel 3 ; southwestern Puerto Rico ; ocean tidal backwater ; stage–discharge relation ; ocean tide model ; Mekong Delta ; suspended particulate matter ; ocean color data ; satellite remote sensing ; in situ measurements ; C2RCC ; Landsat-8 OLI ; Sentinel-2 MSI ; Mzymta River ; Black Sea ; MUR SST ; SST fronts ; Inner Sea of Chiloé ; northern Patagonia ; suspended sediment ; Typhoon Soudelor ; spatial–temporal distribution ; HF marine radars ; wave energy ; thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
    Language: English
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  • 3
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    MDPI - Multidisciplinary Digital Publishing Institute
    Publication Date: 2024-03-23
    Description: This Special Issue is designed to discuss and examine relevant legal issues concerning ocean governance in the context of the United Nations Sustainable Development Goals (SDGs) for the long-lasting benefits of the international community. It will cover, inter alia, the safety of navigation and maritime security, the sustainable use of marine resources (living and non-living), marine environmental protection, climate change, and marine scientific research.
    Keywords: transfer of mining technology ; commercial condition ; protection of intellectual property ; direct technology purchasing ; investment cooperation ; universal jurisdiction ; maritime piracy ; piracy trials ; Somali piracy ; maritime crime ; sustainability ; community interests ; marine genetic resources ; common heritage of mankind ; BBNJ ; integrated coastal management ; land and sea coordination ; ecological environment ; ocean law ; sustainable development ; fishery resources ; community interest ; international cooperation ; climate change ; fishery management ; legal principles ; LOSC ; precautionary approach ; ecosystem ; seasonal closure ; CCAMLR ; MPAs ; RFMOs ; conservation measures ; China ; ocean governance ; sustainable development goals (SDGs) ; SDG 14 ; marine environment ; international environmental law ; Law of the Sea ; ocean acidification ; rising-sea-levels ; meta-governance ; ocean action ; global environment ; regulatory governance ; IMO ; China’s role ; submissions’ adoption ; law of the sea ; deep seabed mining ; national legislation ; sponsoring state ; marine ecological environment ; multiple subjects ; co-management ; ocean community with a shared future ; cruise ships ; public health emergency of international concern (PHEIC) ; international obligations ; rule of law ; COVID-19 ; China’s white paper for Arctic policy ; fisheries resources ; Arctic Ocean ; Chinese legal rights ; Guangdong-Hong Kong-Macao Greater Bay Area (GBA) ; regional integration and cooperation ; SDGs ; Sanchi ship ; oil spill accident ; marine ecology ; ecological damage compensation ; the precautionary principle ; nuclear safety regulation ; UNCLOS ; international law ; thema EDItEUR::A The Arts
    Language: English
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  • 4
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    MDPI - Multidisciplinary Digital Publishing Institute
    Publication Date: 2023-12-20
    Description: This Special Issue gathers papers reporting research on various aspects of remote sensing of Sea Surface Salinity (SSS) and the use of satellite SSS in oceanography. It includes contributions presenting improvements in empirical or theoretical radiative transfer models; mitigation techniques of external interference such as RFI and land contamination; comparisons and validation of remote sensing products with in situ observations; retrieval techniques for improved coastal SSS monitoring, high latitude SSS and the assessment of ocean interactions with the cryosphere; and data fusion techniques combining SSS with sea surface temperature (SST). New instrument technology for the future of SSS remote sensing is also presented.
    Keywords: Q1-390 ; n/a ; satellite salinity ; one-dimensional (1D) aperture synthesis radiometer ; smos ; Gulf of Maine ; retrieval errors ; Aquarius ; combined active/passive SSS retrieval algorithm ; ocean surface roughness ; upwelling ; salt transport ; quality assessment ; sea ice ; SMOS ; microwave radiometry ; Arctic Gateways ; Aquarius satellite ; validation ; sea surface temperature ; water transport ; forward model ; river discharge ; sea surface salinity ; remote sensing ; retrieval algorithm ; Water Cycle Observation Mission (WCOM) ; SMAP ; microwave remote sensing ; alboran sea ; surface velocity ; Arctic Ocean ; sea surface salinity (SSS) ; coastal ; brightness temperature (TB) ; interferometric microwave imager (IMI) ; Scotian Shelf ; MICAP ; different instrument configurations ; bias characteristics ; mediterranean sea ; Gulf of Mexico ; calibration ; retroflections ; Arctic ocean ; salinity ; Sea Surface Salinity ; Arctic rivers ; Argo ; data processing ; aquarius ; ocean salinity ; Aquarius Validation Data System (AVDS) ; bic Book Industry Communication::G Reference, information & interdisciplinary subjects::GP Research & information: general
    Language: English
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  • 5
    Publication Date: 2023-03-11
    Description: © The Author(s), 2022. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Bullock, E., Kipp, L., Moore, W., Brown, K., Mann, P., Vonk, J., Zimov, N., & Charette, M. Radium inputs into the Arctic Ocean from rivers a basin‐wide estimate. Journal of Geophysical Research: Oceans, 127(9), (2022): e2022JC018964, https://doi.org/10.1029/2022jc018964.
    Description: Radium isotopes have been used to trace nutrient, carbon, and trace metal fluxes inputs from ocean margins. However, these approaches require a full accounting of radium sources to the coastal ocean including rivers. Here, we aim to quantify river radium inputs into the Arctic Ocean for the first time for 226Ra and to refine the estimates for 228Ra. Using new and existing data, we find that the estimated combined (dissolved plus desorbed) annual 226Ra and 228Ra fluxes to the Arctic Ocean are [7.0–9.4] × 1014 dpm y−1 and [15–18] × 1014 dpm y−1, respectively. Of these totals, 44% and 60% of the river 226Ra and 228Ra, respectively are from suspended sediment desorption, which were estimated from laboratory incubation experiments. Using Ra isotope data from 20 major rivers around the world, we derived global annual 226Ra and 228Ra fluxes of [7.4–17] × 1015 and [15–27] × 1015 dpm y−1, respectively. As climate change spurs rapid Arctic warming, hydrological cycles are intensifying and coastal ice cover and permafrost are diminishing. These river radium inputs to the Arctic Ocean will serve as a valuable baseline as we attempt to understand the changes that warming temperatures are having on fluxes of biogeochemically important elements to the Arctic coastal zone.
    Description: This study was a broad, collaborative effort that would not have been possible without contributions from numerous funding sources, including the National Science Foundation (NSF-0751525, NSF-1736277, NSF-1458305, NSF-1938873, NSF-2048067, NSF-2134865), the NERC-BMBF project CACOON [NE/R012806/1] (UKRI NERC) and BMBF-03F0806A, and an EU Starting Grant (THAWSOME-676982).
    Keywords: Radium isotopes ; Arctic Ocean ; River fluxes
    Repository Name: Woods Hole Open Access Server
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  • 6
    Publication Date: 2023-02-28
    Description: Author Posting. © American Geophysical Union, 2022. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 36(8), (2022): e2022GB007320, https://doi.org/10.1029/2022GB007320.
    Description: Biogeochemical cycles in the Arctic Ocean are sensitive to the transport of materials from continental shelves into central basins by sea ice. However, it is difficult to assess the net effect of this supply mechanism due to the spatial heterogeneity of sea ice content. Manganese (Mn) is a micronutrient and tracer which integrates source fluctuations in space and time while retaining seasonal variability. The Arctic Ocean surface Mn maximum is attributed to freshwater, but studies struggle to distinguish sea ice and river contributions. Informed by observations from 2009 IPY and 2015 Canadian GEOTRACES cruises, we developed a three-dimensional dissolved Mn model within a 1/12° coupled ocean-ice model centered on the Canada Basin and the Canadian Arctic Archipelago (CAA). Simulations from 2002 to 2019 indicate that annually, 87%–93% of Mn contributed to the Canada Basin upper ocean is released by sea ice, while rivers, although locally significant, contribute only 2.2%–8.5%. Downstream, sea ice provides 34% of Mn transported from Parry Channel into Baffin Bay. While rivers are often considered the main source of Mn, our findings suggest that in the Canada Basin they are less important than sea ice. However, within the shelf-dominated CAA, both rivers and sediment resuspension are important. Climate-induced disruption of the transpolar drift may reduce the Canada Basin Mn maximum and supply downstream. Other micronutrients found in sediments, such as Fe, may be similarly affected. These results highlight the vulnerability of the biogeochemical supply mechanisms in the Arctic Ocean and the subpolar seas to climatic changes.
    Description: This work was funded by the Natural Sciences and Engineering Research Council of Canada (NSERC) Climate Change and Atmospheric Research Grant: GEOTRACES (RGPCC 433848-12) and VITALS (RGPCC 433898), an NSERC Discovery Grant (RGPIN-2016-03865) to SEA, and by the University of British Columbia through a four year fellowship to BR. Computing resources were provided by Compute Canada (RRG 2648 RAC 2019, RRG 2969 RAC 2020, and RRG 1541 RAC 2021).
    Keywords: GEOTRACES ; Arctic Ocean ; Trace elements ; Canadian Arctic Archipelago ; Ocean modeling ; Micronutrients
    Repository Name: Woods Hole Open Access Server
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  • 7
    Publication Date: 2022-10-26
    Description: Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research-Oceans 124(7), (2019): 4618-4630, doi: 10.1029/2019JC014940.
    Description: The Arctic Ocean mixed layer interacts with the ice cover above and warmer, nutrient‐rich waters below. Ice‐Tethered Profiler observations in the Canada Basin of the Arctic Ocean over 2006–2017 are used to investigate changes in mixed layer properties. In contrast to decades of shoaling since at least the 1980s, the mixed layer deepened by 9 m from 2006–2012 to 2013–2017. Deepening resulted from an increase in mixed layer salinity that also weakened stratification at the base of the mixed layer. Vertical mixing alone can explain less than half of the observed change in mixed layer salinity, and so the observed increase in salinity is inferred to result from changes in freshwater accumulation via changes to ice‐ocean circulation or ice melt/growth and river runoff. Even though salinity increased, the shallowest density surfaces deepened by 5 m on average suggesting that Ekman pumping over this time period remained downward. A deeper mixed layer with weaker stratification has implications for the accessibility of heat and nutrients stored in the upper halocline. The extent to which the mixed layer will continue to deepen appears to depend primarily on the complex set of processes influencing freshwater accumulation.
    Description: We gratefully acknowledge J. Toole for helpful conversations. S. Cole was supported by the National Science Foundation under grant PLR‐1602926 and J. Stadler by the Woods Hole Oceanographic Institution Summer Student Fellowship program. Profile data are available via the Ice‐Tethered Profiler program website: http://whoi.edu/itp. SSM/I ice concentration data were downloaded from the National Snow and Ice Data Center.
    Description: 2019-12-22
    Keywords: Arctic Ocean ; Mixed layer ; Freshwater
    Repository Name: Woods Hole Open Access Server
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  • 8
    Publication Date: 2022-10-26
    Description: © The Author(s), 2020. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in DeGrandpre, M., Evans, W., Timmermans, M., Krishfield, R., Williams, B., & Steele, M. Changes in the arctic ocean carbon cycle with diminishing ice cover. Geophysical Research Letters, 47(12), (2020): e2020GL088051, doi:10.1029/2020GL088051.
    Description: Less than three decades ago only a small fraction of the Arctic Ocean (AO) was ice free and then only for short periods. The ice cover kept sea surface pCO2 at levels lower relative to other ocean basins that have been exposed year round to ever increasing atmospheric levels. In this study, we evaluate sea surface pCO2 measurements collected over a 6‐year period along a fixed cruise track in the Canada Basin. The measurements show that mean pCO2 levels are significantly higher during low ice years. The pCO2 increase is likely driven by ocean surface heating and uptake of atmospheric CO2 with large interannual variability in the contributions of these processes. These findings suggest that increased ice‐free periods will further increase sea surface pCO2, reducing the Canada Basin's current role as a net sink of atmospheric CO2.
    Description: This research was made possible by grants from the NSF Arctic Observing Network program (ARC‐1107346, PLR‐1302884, PLR‐1504410, and OPP‐1723308). In addition, M. S. was supported by ONR (Grant 00014‐17‐1‐2545), NASA (Grant NNX16AK43G), and NSF (Grants PLR‐1503298 and OPP‐1751363).
    Keywords: Arctic Ocean ; Ice concentration ; Seawater CO2 ; Interannual variability ; Canada Basin ; Shipboard CO2 measurements
    Repository Name: Woods Hole Open Access Server
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  • 9
    Publication Date: 2022-10-26
    Description: Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research-Oceans 124(5), (2019): 3279-3297, doi: 10.1029/2019JC014988.
    Description: Radium isotopes are produced through the decay of thorium in sediments and are soluble in seawater; thus, they are useful for tracing ocean boundary‐derived inputs to the ocean. Here we apply radium isotopes to study continental inputs and water residence times in the Arctic Ocean, where land‐ocean interactions are currently changing in response to rising air and sea temperatures. We present the distributions of radium isotopes measured on the 2015 U.S. GEOTRACES transect in the Western Arctic Ocean and combine this data set with historical radium observations in the Chukchi Sea and Canada Basin. The highest activities of radium‐228 were observed in the Transpolar Drift and the Chukchi shelfbreak jet, signaling that these currents are heavily influenced by interactions with shelf sediments. The ventilation of the halocline with respect to inputs from the Chukchi shelf occurs on time scales of ≤19–23 years. Intermediate water ventilation time scales for the Makarov and Canada Basins were determined to be ~20 and 〉30 years, respectively, while deep water residence times in these basins were on the order of centuries. The radium distributions and residence times described in this study serve as a baseline for future studies investigating the impacts of climate change on the Arctic Ocean.
    Description: We thank the captain and crew of the USCGC Healy (HLY1502) and the chief scientists D. Kadko and W. Landing for coordinating a safe and successful expedition. We thank the members of the pump team, P. Lam, E. Black, S. Pike, X. Yang, and M. Heller for their assistance with sample collection and for their unfailingly positive attitudes during this 65‐day expedition. We also appreciate sampling assistance from P. Aguilar and M. Stephens, and MATLAB assistance from B. Corlett, A. Pacini, P. Lin, and M. Li. The radium data from the HLY1502 expedition are available through the Biological & Chemical Oceanography Data Management Office (https://www.bco‐dmo.org/dataset/718440) and the radium measurements from the SHEBA, AWS‐2000, and SBI expeditions can be found in the supporting information. This work was funded by NSF awards OCE‐1458305 to M.A.C., OCE‐1458424 to W.S.M., and PLR‐1504333 to R.S.P. This research was conducted with Government support under and awarded by a DoD, Air Force Office of Scientific Research, National Defense Science and Engineering Graduate (NDSEG) Fellowship awarded to L.E.K., 32 CFR 168a.
    Description: 2019-10-26
    Keywords: Radium ; Arctic Ocean ; GEOTRACES ; Chukchi shelf
    Repository Name: Woods Hole Open Access Server
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  • 10
    Publication Date: 2022-10-26
    Description: Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 126(7), (2021): e2021JC017407, https://doi.org/10.1029/2021JC017407.
    Description: The Arctic Ocean receives a large supply of dissolved organic matter (DOM) from its catchment and shelf sediments, which can be traced across much of the basin's upper waters. This signature can potentially be used as a tracer. On the shelf, the combination of river discharge and sea-ice formation, modifies water densities and mixing considerably. These waters are a source of the halocline layer that covers much of the Arctic Ocean, but also contain elevated levels of DOM. Here we demonstrate how this can be used as a supplementary tracer and contribute to evaluating ocean circulation in the Arctic. A fraction of the organic compounds that DOM consists of fluoresce and can be measured using in-situ fluorometers. When deployed on autonomous platforms these provide high temporal and spatial resolution measurements over long periods. The results of an analysis of data derived from several Ice Tethered Profilers (ITPs) offer a unique spatial coverage of the distribution of DOM in the surface 800 m below Arctic sea-ice. Water mass analysis using temperature, salinity and DOM fluorescence, can clearly distinguish between the contribution of Siberian terrestrial DOM and marine DOM from the Chukchi shelf to the waters of the halocline. The findings offer a new approach to trace the distribution of Pacific waters and its export from the Arctic Ocean. Our results indicate the potential to extend the approach to separate freshwater contributions from, sea-ice melt, riverine discharge and the Pacific Ocean.
    Description: Danish Strategic Research Council for the NAACOS project (grant no. 10-093903), the Danish Center for Marine Research (grant no. 2012-01). C. A. S. has received funding from the Independent Research Fund Denmark Grant No. 9040-00266B. Funding for R.M.W.A. came from the US NSF, Arctic Natural Science program grant 1504469. RG-A has received funding from the European Union's Horizon 2020 research and innovation program under the Marie Skłodowska-Curie Grant Agreement No. 839311. ITP93 and part of the work by MH and BR were a contribution to the Helmholtz society strategic investment Frontiers in Arctic Marine monitoring (FRAM). The work of BR is a contribution to the cooperative projects Regional Atlantic Circulation and global Change (RACE) grant #03F0824E funded by the German Ministry of Science and Education (BBMF) and Advective Pathways of nutrients and key Ecological substances in the Arctic (APEAR) grants NE/R012865/1, NE/R012865/2 and #03V01461, part of the Changing Arctic Ocean program, jointly funded by the UKRI Natural Environment Research Council (NERC) and the BMBF. Support for Krishfield was made possible by grants from the NSF Arctic Observing Network program (PLR-1303644 and OPP-1756100).
    Description: 2021-12-27
    Keywords: Arctic Ocean ; CDOM ; DOM ; FDOM ; Fluorescence ; Halocline
    Repository Name: Woods Hole Open Access Server
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