Sebastian Mernild

Last updated
IMBIE Team (2020). "Mass balance of the Greenland Ice Sheet from 1992 to 2018". Nature . Ice Sheet Mass Balance Inter-comparison Exercise (IMBIE). 579 (7798): 233–239. doi:10.1038/s41586-019-1855-2. hdl: 1874/407943 . ISSN   1476-4687. PMID   31822019. S2CID   219146922.Wikidata-logo.svg Wikidata ()
  • Lead author: Snow, Water, Ice and Permafrost in the Arctic (SWIPA) 2017 (Report). Vol. XIV. Oslo: [[Arctic Council#Working groups, programs and action plans|Arctic Monitoring and Assessment Programme (AMAP)]]. 2017. ISBN   978-82-7971-101-8.
  • Contributing author: The Arctic Freshwater System in a Changing Climate (Report). WCRP Climate and Cryosphere (CliC) Project, Arctic Monitoring and Assessment Programme (AMAP), International Arctic Science Committee (IASC). 2016. ISBN   978-82-7971-097-4. OCLC   981102448.
  • Author: Arctic Report Card 2012 (Report). Washington, D.C.: National Oceanic and Atmospheric Administration - Arctic Report Card. 2013. OCLC   951586159.Wikidata-logo.svg Wikidata ()
  • Author: Arctic Report Card 2011 (Report). Washington, D.C.: National Oceanic and Atmospheric Administration - Arctic Report Card. 2012. OCLC   1059243645.Wikidata-logo.svg Wikidata ()
  • Lead author: Melting snow and ice: a call for action (Report). Center for Ice, Climate and Ecosystems, Norwegian Polar Institute. 2009. ISBN   978-82-7666-264-1. OCLC   770710446.
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    Related Research Articles

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    Greenland is located between the Arctic Ocean and the North Atlantic Ocean, northeast of Canada and northwest of Iceland. The territory comprises the island of Greenland—the largest island in the world—and more than a hundred other smaller islands. Greenland has a 1.2 kilometre long border with Canada on Hans Island. A sparse population is confined to small settlements along certain sectors of the coast. Greenland possesses the world's second-largest ice sheet.

    <span class="mw-page-title-main">Cryosphere</span> Those portions of Earths surface where water is in solid form

    The cryosphere is an all-encompassing term for the portions of Earth's surface where water is in solid form, including sea ice, lake ice, river ice, snow cover, glaciers, ice caps, ice sheets, and frozen ground. Thus, there is a wide overlap with the hydrosphere. The cryosphere is an integral part of the global climate system with important linkages and feedbacks generated through its influence on surface energy and moisture fluxes, clouds, precipitation, hydrology, atmospheric and oceanic circulation.

    <span class="mw-page-title-main">Ice shelf</span> Large floating platform of ice caused by glacier flowing onto ocean surface

    An ice shelf is a large floating platform of ice that forms where a glacier or ice sheet flows down to a coastline and onto the ocean surface. Ice shelves are only found in Antarctica, Greenland, Northern Canada, and the Russian Arctic. The boundary between the floating ice shelf and the anchor ice that feeds it is the grounding line. The thickness of ice shelves can range from about 100 m (330 ft) to 1,000 m (3,300 ft).

    <span class="mw-page-title-main">Byrd Polar and Climate Research Center</span>

    The Byrd Polar and Climate Research Center (BPCRC) is a polar, alpine, and climate research center at The Ohio State University founded in 1960.

    <span class="mw-page-title-main">Ice cap</span> Ice mass that covers less than 50,000 km² of land area

    In glaciology, an ice cap is a mass of ice that covers less than 50,000 km2 (19,000 sq mi) of land area. Larger ice masses covering more than 50,000 km2 (19,000 sq mi) are termed ice sheets.

    <span class="mw-page-title-main">Greenland ice sheet</span> Vast body of ice in Greenland

    The Greenland ice sheet is a vast body of ice covering 1,710,000 square kilometres (660,000 sq mi), roughly near 80% of the surface of Greenland. It is sometimes referred to as an ice cap, or under the term inland ice, or its Danish equivalent, indlandsis. The acronym GIS is frequently used in the scientific literature.

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    <span class="mw-page-title-main">Tipping points in the climate system</span> Large and possibly irreversible changes in the climate system

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    <span class="mw-page-title-main">Ice–albedo feedback</span> Positive feedback climate process

    Ice–albedo feedback is a positive feedback climate process where a change in the area of ice caps, glaciers, and sea ice alters the albedo and surface temperature of a planet. Ice is very reflective, therefore it reflects far more solar energy back to space than the other types of land area or open water. Ice–albedo feedback plays an important role in global climate change. For instance, at higher latitudes, warmer temperatures melt the ice sheets. However, if warm temperatures decrease the ice cover and the area is replaced by water or land, the albedo would decrease. This increases the amount of solar energy absorbed, leading to more warming. The change in albedo acts to reinforce the initial alteration in ice area leading to more warming. Warming tends to decrease ice cover and hence decrease the albedo, increasing the amount of solar energy absorbed and leading to more warming. In the geologically recent past, the ice–albedo positive feedback has played a major role in the advances and retreats of the Pleistocene ice sheets. Inversely, cooler temperatures increase ice, which increases albedo, leading to more cooling.

    <span class="mw-page-title-main">Frank Pattyn</span> Belgian glaciologist

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    Sebastian H. Mernild
    Pro-Vice-Chancellor of the University of Southern Denmark
    Assumed office
    October 2020