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Dissertations / Theses on the topic 'Sea-ice melt'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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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10

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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11

Kirk, Robert B. "The optical and microwave properties of melt ponds over first year Arctic sea ice." 2005. http://hdl.handle.net/1993/20148.

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12

Rossnagel, Andrea L. "Spatial and temporal changes of photosynthetically available radiation, temperature and salinity beneath a variable sea ice cover." 2012. http://hdl.handle.net/1993/5090.

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Melt ponds greatly increase the transmission of solar radiation through sea ice relative to snow covered or bare ice. This rise in transmittance has the potential to enhance water column heating and primary production. I examine how spatially variable sea ice surfaces control the under-ice salinity, temperature and photosynthetically active radiation (PAR) and provide estimates of solar heating and primary production during melt. Conductivity, temperature and PAR profiles were measured in the Canadian Arctic under snow covered ice, leads, bare ice and melt ponds. The under-ice light field to a

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13

Wiederwohl, Christina 1980. "The Ross Sea Response to Evolving Ocean-Ice Interactions in a Changing Climate." Thesis, 2012. http://hdl.handle.net/1969.1/148296.

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Early 1990s to late 2000s freshening (ΔS ≈ -0.001–0.002) and warming (Δθ ≈ 0.02°C–0.035°C) of bottom waters was detected in the southern Pacific Ocean, and Ross Sea source waters progressively freshened during the past four decades. This study investigates potential freshwater anomaly sources and quantifies their effect. Glacial melt water inputs to the GCT increased by 1.3 km^3 per decade (1976– 2007), more rapidly so after 2000 (6.8 km^3 per decade), freshening local Shelf Water by 0.0004 per decade. Lighter basal melt inputs to the LAT started in 1994 and also picked up after 2000 to 14.9

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14

Tan, Wenxia. "An Examination of Sea Ice Spring and Summer Retreat in the Canadian Arctic Archipelago: 1989 to 2010." Thesis, 2013. http://hdl.handle.net/10012/7724.

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The sea ice extent change and variability of the Canadian Arctic Archipelago (CAA) are quite different compared to the Arctic as a whole due to its unique geographic settings. In this thesis, the sea ice retreat processes, the connection with other Arctic regions, and the linkages to the surface radiation flux in the CAA are examined. The sea ice retreat processes in the CAA follow a four-phase process: a slow ice melt phase that usually lasts until early June (phase 1); a quick melt phase with large daily sea ice extent change which lasts close to half-a-month (phase 2); a slow melt phase

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15

Moorman, Ruth. "Response of Antarctic ocean circulation to increased meltwater." Thesis, 2019. http://hdl.handle.net/1885/187134.

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The implications of ocean freshening from accelerating Antarctic land-ice loss are poorly understood, due to the scarcity of observations near the Antarctic coast, and the high spatial and temporal resolution required to resolve Antarctic continental shelf processes in ocean models. Here, a high-resolution global ocean--sea-ice model is used to investigate the response of Antarctic continental shelf circulation to increasing meltwater. Two freshwater perturbation experiments are conducted, using projected Antarctic ice-loss rates under RCP 4.5 and RCP 8.5 emissions scenarios at 2100.We find th

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16

García, Rodríguez Nuria. "A problemática do Ártico na atualidade : uma visão estratégica." Master's thesis, 2019. http://hdl.handle.net/10400.14/31477.

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O processo de transformação que se verifica nos últimos anos no Ártico, não é mais do que tem acontecido nas duas últimas décadas, com a única diferença de que o degelo tem vindo a acentuar-se e a diminuição da cobertura de gelo marinho afetou significativamente as populações, a fauna e a flora da região. O que para uns, significa maiores e melhores comunicações pelas “novas” rotas marítimas durante períodos de tempo mais alargados, bem como mais fácil acesso às reservas de recursos naturais até então inexplorados, para outros o degelo significa, poluição, a perda cada vez maior da bio

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