Relevant bibliographies by topics / Sea-ice melt

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Sea-ice melt'

Author: Grafiati
Published: 2 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Sea-ice melt"

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Stroeve, Julienne C., John R. Mioduszewski, Asa Rennermalm, Linette N. Boisvert, Marco Tedesco, and David Robinson. "Investigating the local-scale influence of sea ice on Greenland surface melt." Cryosphere 11, no. 5 (2017): 2363–81. http://dx.doi.org/10.5194/tc-11-2363-2017.

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Abstract. Rapid decline in Arctic sea ice cover in the 21st century may have wide-reaching effects on the Arctic climate system, including the Greenland ice sheet mass balance. Here, we investigate whether local changes in sea ice around the Greenland ice sheet have had an impact on Greenland surface melt. Specifically, we investigate the relationship between sea ice concentration, the timing of melt onset and open-water fraction surrounding Greenland with ice sheet surface melt using a combination of remote sensing observations, and outputs from a reanalysis model and a regional climate model
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Diamond, Rachel, Louise C. Sime, David Schroeder, and Maria-Vittoria Guarino. "The contribution of melt ponds to enhanced Arctic sea-ice melt during the Last Interglacial." Cryosphere 15, no. 11 (2021): 5099–114. http://dx.doi.org/10.5194/tc-15-5099-2021.

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Abstract. The Hadley Centre Global Environment Model version 3 (HadGEM3) is the first coupled climate model to simulate an ice-free Arctic during the Last Interglacial (LIG), 127 000 years ago. This simulation appears to yield accurate Arctic surface temperatures during the summer season. Here, we investigate the causes and impacts of this extreme simulated ice loss. We find that the summer ice melt was predominantly driven by thermodynamic processes: atmospheric and ocean circulation changes did not significantly contribute to the ice loss. We demonstrate these thermodynamic processes were si
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Kern, Stefan, Anja Rösel, Leif Toudal Pedersen, Natalia Ivanova, Roberto Saldo, and Rasmus Tage Tonboe. "The impact of melt ponds on summertime microwave brightness temperatures and sea-ice concentrations." Cryosphere 10, no. 5 (2016): 2217–39. http://dx.doi.org/10.5194/tc-10-2217-2016.

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Abstract. Sea-ice concentrations derived from satellite microwave brightness temperatures are less accurate during summer. In the Arctic Ocean the lack of accuracy is primarily caused by melt ponds, but also by changes in the properties of snow and the sea-ice surface itself. We investigate the sensitivity of eight sea-ice concentration retrieval algorithms to melt ponds by comparing sea-ice concentration with the melt-pond fraction. We derive gridded daily sea-ice concentrations from microwave brightness temperatures of summer 2009. We derive the daily fraction of melt ponds, open water betwe
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West, Alex, Edward Blockley, and Matthew Collins. "Understanding model spread in sea ice volume by attribution of model differences in seasonal ice growth and melt." Cryosphere 16, no. 10 (2022): 4013–32. http://dx.doi.org/10.5194/tc-16-4013-2022.

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Abstract. Arctic sea ice is declining rapidly, but predictions of its future loss are made difficult by the large spread both in present-day and in future sea ice area and volume; hence, there is a need to better understand the drivers of model spread in sea ice state. Here we present a framework for understanding differences between modelled sea ice simulations based on attributing seasonal ice growth and melt differences. In the method presented, the net downward surface flux is treated as the principal driver of seasonal sea ice growth and melt. An energy balance approach is used to estimat
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Geilfus, N. X., R. J. Galley, O. Crabeck, et al. "Inorganic carbon dynamics of melt pond-covered first year sea ice in the Canadian Arctic." Biogeosciences Discussions 11, no. 5 (2014): 7485–519. http://dx.doi.org/10.5194/bgd-11-7485-2014.

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Abstract. Melt pond formation is a common feature of the spring and summer Arctic sea ice. However, the role of the melt ponds formation and the impact of the sea ice melt on both the direction and size of CO2 flux between air and sea is still unknown. Here we describe the CO2-carbonate chemistry of melting sea ice, melt ponds and the underlying seawater associated with measurement of CO2 fluxes across first year landfast sea ice in the Resolute Passage, Nunavut, in June 2012. Early in the melt season, the increase of the ice temperature and the subsequent decrease of the bulk ice salinity pro
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Liang, Hongjie, and Wen Zhou. "Dynamic and thermodynamic processes related to sea-ice surface melt advance in the Laptev Sea and East Siberian Sea." Cryosphere 18, no. 8 (2024): 3559–69. http://dx.doi.org/10.5194/tc-18-3559-2024.

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Abstract. Arctic summer sea ice has shrunk considerably in recent decades. This study investigates springtime sea-ice surface melt onset in the Laptev Sea and East Siberian Sea, which are key seas along the Northeast Passage. Instead of region-mean melt onset, we define an index of melt advance, which is the areal percentage of a sea that has experienced sea-ice surface melting before the end of May. Four representative scenarios of melt advance in the region are identified. Each scenario is accompanied by a combination of distinct patterns between atmospheric circulation, atmospheric thermody
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Bates, N. R., R. Garley, K. E. Frey, K. L. Shake, and J. T. Mathis. "Sea-ice melt CO<sub>2</sub>-carbonate chemistry in the western Arctic Ocean: meltwater contributions to air-sea CO<sub>2</sub> gas exchange, mixed layer properties and rates of net community production under sea ice." Biogeosciences Discussions 11, no. 1 (2014): 1097–145. http://dx.doi.org/10.5194/bgd-11-1097-2014.

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Abstract. The carbon dioxide (CO2)-carbonate chemistry of sea-ice melt and co-located, contemporaneous seawater has rarely been studied in sea ice covered oceans. Here, we describe the CO2-carbonate chemistry of sea-ice melt (both above sea ice as "melt ponds" and below sea ice as "interface waters") and mixed layer properties in the western Arctic Ocean in the early summer of 2010 and 2011. At nineteen stations, the salinity (~ 0.5 to &lt; 6.5), dissolved inorganic carbon (DIC; ~ 20 to &lt; 550 μmol kg–1) and total alkalinity (TA; ~ 30 to &lt; 500 μmol kg–1) of above-ice melt pond water was l
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Hohenegger, C., B. Alali, K. R. Steffen, D. K. Perovich, and K. M. Golden. "Transition in the fractal geometry of Arctic melt ponds." Cryosphere Discussions 6, no. 3 (2012): 2161–77. http://dx.doi.org/10.5194/tcd-6-2161-2012.

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Abstract. During the Arctic melt season, the sea ice surface undergoes a remarkable transformation from vast expanses of snow covered ice to complex mosaics of ice and melt ponds. Sea ice albedo, a key parameter in climate modeling, is determined by the complex evolution of melt pond configurations. In fact, ice-albedo feedback has played a major role in the recent declines of the summer Arctic sea ice pack. However, understanding melt pond evolution remains a significant challenge to improving climate projections. By analyzing area-perimeter data from hundreds of thousands of melt ponds, we f
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Hohenegger, C., B. Alali, K. R. Steffen, D. K. Perovich, and K. M. Golden. "Transition in the fractal geometry of Arctic melt ponds." Cryosphere 6, no. 5 (2012): 1157–62. http://dx.doi.org/10.5194/tc-6-1157-2012.

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Abstract. During the Arctic melt season, the sea ice surface undergoes a remarkable transformation from vast expanses of snow covered ice to complex mosaics of ice and melt ponds. Sea ice albedo, a key parameter in climate modeling, is determined by the complex evolution of melt pond configurations. In fact, ice–albedo feedback has played a major role in the recent declines of the summer Arctic sea ice pack. However, understanding melt pond evolution remains a significant challenge to improving climate projections. By analyzing area–perimeter data from hundreds of thousands of melt ponds, we f
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Wang, Mingfeng, Felix Linhardt, Victor Lion, and Natascha Oppelt. "Melt Pond Evolution along the MOSAiC Drift: Insights from Remote Sensing and Modeling." Remote Sensing 16, no. 19 (2024): 3748. http://dx.doi.org/10.3390/rs16193748.

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Melt ponds play a crucial role in the melting of Arctic sea ice. Studying the evolution of melt ponds is essential for understanding changes in Arctic sea ice. In this study, we used a revised sea ice model to simulate the evolution of melt ponds along the MOSAiC drift at a resolution of 10 m. A novel melt pond parameterization scheme simulates the movement of meltwater under the influence of gravity over a realistic sea ice topography. We evaluated different melt pond parameterization schemes based on remote sensing observations. The absolute deviation of the maximum pond coverage simulated b
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Dissertations / Theses on the topic "Sea-ice melt"

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Nasonova, Sasha. "Estimating Arctic sea ice melt pond fraction and assessing ice type separability during advanced melt." Thesis, Remote Sensing, 2017. https://dspace.library.uvic.ca//handle/1828/9313.

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Arctic sea ice is rapidly declining in extent, thickness, volume and age, with the majority of the decline in extent observed at the end of the melt season. Advanced melt is a thermodynamic regime and is characterized by the formation of melt ponds on the sea ice surface, which have a lower surface albedo (0.2-0.4) than the surrounding ice (0.5-0.7) allowing more shortwave radiation to enter the system. The loss of multiyear ice (MYI) may have a profound impact on the energy balance of the system because melt ponds on first-year ice (FYI) comprise up to 70% of the ice surface during advanced m
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Guo, Wenkai. "The relationship between sea ice retreat and Greenland ice sheet surface-melt." The Ohio State University, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=osu1397692613.

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Taylor, Paul Duncan. "Mathematical modelling the formation and evolution of melt ponds on sea ice." Thesis, University College London (University of London), 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.406901.

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Nicolaus, Marcel. "Beobachtung und Modellierung der Schneeschmelze und Aufeisbildung auf arktischem und antarktischem Meereis = Observation and modelling of snow melt and superimposed ice formation on Arctic and Antarctic sea ice /." Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung, 2006. http://www.gbv.de/dms/bs/toc/518226271.pdf.

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De, Abreu Roger A. "In situ and satellite observations of the visible and infrared albedo of sea ice during spring melt." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/nq21339.pdf.

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Kunz, Lukas Brad. "A New Method for Melt Detection on Antarctic Ice-Shelves and Scatterometer Calibration Verification." Diss., CLICK HERE for online access, 2004. http://contentdm.lib.byu.edu/ETD/image/etd527.pdf.

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König, Marcel [Verfasser], Natascha [Akademischer Betreuer] Oppelt, and Peter [Gutachter] Gege. "Mapping Melt Pond Bathymetry on Arctic Sea Ice by Means of Optical Remote Sensing / Marcel König ; Gutachter: Peter Gege ; Betreuer: Natascha Oppelt." Kiel : Universitätsbibliothek Kiel, 2021. http://d-nb.info/1234451379/34.

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Mortin, Jonas. "On the Arctic Seasonal Cycle." Doctoral thesis, Stockholms universitet, Meteorologiska institutionen (MISU), 2014. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-100008.

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The seasonal cycle of snow and sea ice is a fundamental feature of the Arctic climate system. In the Northern Hemisphere, about 55 million km2 of sea ice and snow undergo complete melt and freeze processes every year. Because snow and sea ice are much brighter (higher albedo) than the underlying surface, their presence reduces absorption of incoming solar energy at high latitudes. Therefore, changes of the sea-ice and snow cover have a large impact on the Arctic climate and possibly at lower latitudes. One of the most important determining factors of the seasonal snow and sea-ice cover is the
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Kuo, Li-Chieh, and 郭立婕. "Impact of Arctic Sea Ice Melt On Global Ocean Transportation." Thesis, 2016. http://ndltd.ncl.edu.tw/handle/27014838436251147639.

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碩士<br>國立中興大學<br>國際政治研究所<br>104<br>With the global warming , the attention to the Arctic region is gradually increasing, however, in addition to the attention of the environment, the interest of transportation is also one of the concerns. As the ice melts, the likelihood of using the Arctic Route all year round increases dramatically. With the qualitative research method and quantitative research method, we research the situation from political and economic aspects, first of all, from the political aspect, we observed the governance situations in Arctic region and the how Arctic countries think
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Amundrud, Trisha Lynne. "Geometrical constraints on the formation and melt of ridged sea ice." Thesis, 2005. http://hdl.handle.net/2429/16976.

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The Arctic ice pack consists of flat level ice, open water, and large ridge structures. During winter, ice thickens and is compacted into ridges, increasing the Arctic ice volume. In summer, ridging is accompanied by ice melt processes, which act to decrease ice volume. Current ice-atmosphere-ocean models cannot reproduce the evolution of the ridged ice fraction, suggesting that ridging or melt may be inappropriately parameterized. To increase our understanding of ridged ice evolution, this thesis investigates the factors that constrain the ridging and melt processes. A unique ice draft dist
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Books on the topic "Sea-ice melt"

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Rösel, Anja. Detection of Melt Ponds on Arctic Sea Ice with Optical Satellite Data. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-37033-5.

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Nikolaus, Marcel. Beobachtung und Modellierung der Schneeschmelze und Aufeisbildung auf arktischem und antarktischem Meereis: Observation and modelling of snow melt and superimposed ice formation on Arctic and Antarctic sea ice. Alfred-Wegener-Institut für Polar- und Meeresforschung, 2006.

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Rösel, Anja. Detection of Melt Ponds on Arctic Sea Ice with Optical Satellite Data. Springer, 2013.

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Rösel, Anja. Detection of Melt Ponds on Arctic Sea Ice with Optical Satellite Data. Springer London, Limited, 2013.

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Buschmann, Rainer F., and Lance Nolde, eds. The World’s Oceans. ABC-CLIO, 2018. http://dx.doi.org/10.5040/9798216039464.

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This single-volume resource explores the five major oceans of the world, addressing current issues such as sea rise and climate change and explaining the significance of the oceans from historical, geographic, and cultural perspectives. The World’s Oceans: Geography, History, and Environment is a one-stop resource that describes in-depth the Arctic, Atlantic, Indian, Pacific, and Southern Oceans and identifies their importance, today and throughout history. Essays address the subject areas of oceans and seas in world culture, fishing and shipping industries through history, ocean exploration,
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Zellen, Barry Scott. Arctic Doom, Arctic Boom. ABC-CLIO, LLC, 2009. http://dx.doi.org/10.5040/9798400614132.

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An expert examination of the way climate change is transforming the Arctic environmentally, economically, and geopolitically, and how the challenges of that transformation should be met. A growing number of scientists estimate that there will be no summer ice in the Arctic by as soon as 2013. Are we approaching the "End of the Arctic?" as journalist Ed Struzik asked in 1992, or fully entering the "Age of the Arctic," as Arctic expert Oran Young predicted in 1986? Arctic Doom, Arctic Boom: The Geopolitics of Climate Change in the Arctic looks at the uncertainty at the top of the world as the sh
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Book chapters on the topic "Sea-ice melt"

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Rösel, Anja. "Physical Characteristics of Sea Ice." In Detection of Melt Ponds on Arctic Sea Ice with Optical Satellite Data. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-37033-5_2.

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Steele, Michael, and Gregory M. Flato. "Sea Ice Growth, Melt, and Modeling: A Survey." In The Freshwater Budget of the Arctic Ocean. Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-011-4132-1_23.

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Gogineni, S. Prasad, Richard K. Moore, Thomas C. Grenfell, D. G. Barber, Susan Digby, and Mark Drinkwater. "The effects of freeze-up and melt processes on microwave signatures." In Microwave Remote Sensing of Sea Ice. American Geophysical Union, 1992. http://dx.doi.org/10.1029/gm068p0329.

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Garrity, Caren. "Characterization of snow on floating ice and case studies of brightness temperature changes during the onset of melt." In Microwave Remote Sensing of Sea Ice. American Geophysical Union, 1992. http://dx.doi.org/10.1029/gm068p0313.

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Rösel, Anja. "Melt Pond Determination from MODIS Data." In Detection of Melt Ponds on Arctic Sea Ice with Optical Satellite Data. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-37033-5_5.

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Rösel, Anja. "Melt Pond Determination from Landsat Satellite Data." In Detection of Melt Ponds on Arctic Sea Ice with Optical Satellite Data. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-37033-5_4.

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Scagliarini, Andrea, Enrico Calzavarini, Daniela Mansutti, and Federico Toschi. "Modelling Sea Ice and Melt Ponds Evolution: Sensitivity to Microscale Heat Transfer Mechanisms." In Mathematical Approach to Climate Change and its Impacts. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-38669-6_6.

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Rösel, Anja. "Introduction." In Detection of Melt Ponds on Arctic Sea Ice with Optical Satellite Data. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-37033-5_1.

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Rösel, Anja. "Optical Remote Sensing." In Detection of Melt Ponds on Arctic Sea Ice with Optical Satellite Data. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-37033-5_3.

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Rösel, Anja. "Summary and Outlook." In Detection of Melt Ponds on Arctic Sea Ice with Optical Satellite Data. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-37033-5_6.

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Conference papers on the topic "Sea-ice melt"

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Li, Xudong, and Chuan Xiong. "Estimating Arctic Sea Ice Melt Pond Depth and Water Volume with Optical Satellite Imagery." In IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2024. http://dx.doi.org/10.1109/igarss53475.2024.10641649.

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Lu, Xiaomei, and Yongxiang Hu. "Sea ice melt and freeze onset from space-based lidar measurements." In IGARSS 2020 - 2020 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2020. http://dx.doi.org/10.1109/igarss39084.2020.9323557.

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Frantz, Carie M., Bonnie Light, Bonnie Light, et al. "ROTTEN ICE: STRUCTURAL AND BIOLOGICAL CHANGES IN FIRST-YEAR ARCTIC SEA ICE DURING ADVANCED SUMMER MELT." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285390.

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Rosel, Anja, and Lars Kaleschke. "Influence of melt ponds on microwave sensors' sea ice concentration retrieval algorithms." In IGARSS 2012 - 2012 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2012. http://dx.doi.org/10.1109/igarss.2012.6350608.

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Hicks, B., and D. Long. "Diurnal Melt Detection on Arctic Sea Ice Using Tandem QuikSCAT and SeaWinds Data." In 2006 IEEE International Symposium on Geoscience and Remote Sensing. IEEE, 2006. http://dx.doi.org/10.1109/igarss.2006.1054.

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Perovich, Donald K., and John W. Govoni. "Light reflection from a sea-ice cover during the onset of summer melt." In San Diego '92, edited by Gary D. Gilbert. SPIE, 1992. http://dx.doi.org/10.1117/12.140681.

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Marks, Henrik, Georg Heygster, and Larysa Istomina. "Cloud filtering with MERIS and AATSR for melt pond detection on Arctic sea ice." In IGARSS 2016 - 2016 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2016. http://dx.doi.org/10.1109/igarss.2016.7731000.

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Devnath, Maloy Kumar, Sudip Chakraborty, and Vandana P. Janeja. "CMAD: Advancing Understanding of Geospatial Clusters of Anomalous Melt Events in Sea Ice Extent." In SIGSPATIAL '24: The 32nd ACM International Conference on Advances in Geographic Information Systems. ACM, 2024. http://dx.doi.org/10.1145/3678717.3691280.

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Illarionova, Margarita, and Margarita Illarionova. "THE INFLUENCE OF SEA ICE ON THE SEA COAST OF SHANTAR ISLANDS." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b9399a9be55.67359338.

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The Shantar Islands is the group of islands satiated in the Sea of Okhotsk near the exit of Uda Bay, Tugur Bay and Ulban Bay. The islands separated from the mainland and started to exist only 6000 years ago. It happened under the influence of the sea transgression followed by flooding of some parts of the land surface and isolation of the most elevated mountain parts from the mainland. The climate of The Shantar Island is more severe than the climate in the North part of the Sea of Okhotsk due to its proximity to cold regions of Yakutia, complex system of wind and tidal currents, the duration
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Illarionova, Margarita, and Margarita Illarionova. "THE INFLUENCE OF SEA ICE ON THE SEA COAST OF SHANTAR ISLANDS." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4315b18932.

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The Shantar Islands is the group of islands satiated in the Sea of Okhotsk near the exit of Uda Bay, Tugur Bay and Ulban Bay. The islands separated from the mainland and started to exist only 6000 years ago. It happened under the influence of the sea transgression followed by flooding of some parts of the land surface and isolation of the most elevated mountain parts from the mainland. The climate of The Shantar Island is more severe than the climate in the North part of the Sea of Okhotsk due to its proximity to cold regions of Yakutia, complex system of wind and tidal currents, the duration
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Reports on the topic "Sea-ice melt"

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Douglas, Thomas, Matthew Sturm, Joel Blum, et al. A pulse of mercury and major ions in snowmelt runoff from a small Arctic Alaska watershed. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/41203.

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Atmospheric mercury (Hg) is deposited to Polar Regions during springtime atmospheric mercury depletion events (AMDEs) that require halogens and snow or ice surfaces. The fate of this Hg during and following snowmelt is largely unknown. We measured Hg, major ions, and stable water isotopes from the snowpack through the entire spring melt runoff period for two years. Our small (2.5 ha) watershed is near Barrow (now Utqiaġvik), Alaska. We measured discharge, made 10 000 snow depths, and collected over 100 samples of snow and meltwater for chemical analysis in 2008 and 2009 from the watershed snow
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Goldie, James. The danger as Antarctica's sea ice melts. Monash University, 2024. http://dx.doi.org/10.54377/b969-1e37.

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Jameel, Yusuf, Paul West, and Daniel Jasper. Reducing Black Carbon: A Triple Win for Climate, Health, and Well-Being. Project Drawdown, 2023. http://dx.doi.org/10.55789/y2c0k2p3.

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Black carbon – also referred to as soot – is a particulate matter that results from the incomplete combustion of fossil fuels and biomass. As a major air and climate pollutant, black carbon (BC) emissions have widespread adverse effects on human health and climate change. Globally, exposure to unhealthy levels of particulate matter, including BC, is estimated to cause between three and six million excess deaths every year. These health impacts – and the related economic losses – are felt disproportionately by those living in low- and middle-income countries. Furthermore, BC is a potent greenho
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