Mass balance of the Greenland Ice Sheet from 1992 to 2018

The Greenland Ice Sheet has been a major contributor to global sea-level rise in recent decades1,2, and it is expected to continue to be so3. Although increases in glacier flow4,5,6 and surface melting7,8,9 have been driven by oceanic10,11,12 and atmospheric13,14 warming, the magnitude and trajector...

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Hauptverfasser: Shepherd, Andrew, Ivins, Erik, Rignot, Eric, Smith, Ben, Van Den Broeke, Michiel, Velicogna, Isabella, Whitehouse, Pippa, Briggs, Kate, Joughin, Ian, Krinner, Gerhard, Nowicki, Sophie, Payne, Tony, Scambos, Ted, Schlegel, Nicole, Geruo, A, Agosta, Cécile, Ahlstrøm, Andreas, Babonis, Greg, Barletta, Valentina, Bjørk, Anders A, Blazquez, Alejandro, Bonin, Jennifer, Colgan, William, Csatho, Beata, Cullather, Richard, Engdahl, Marcus E, Felikson, Denis, Fettweis, Xavier, Forsberg, Rene, Hogg, Anna E, Hubert, Gallee, Gardner, Alex, Gilbert, Lin, Gourmelen, Noel, Groh, Andreas, Gunter, Brian, Hanna, Edward, Harig, Christopher, Helm, Veit, Horvath, Alexander, Horwath, Martin, Khan, Shfaqat, Kjeldsen, Kristian K, Hannes, Konrad, Langen, Peter L, Lecavalier, Benoit, Loomis, Bryant, Luthcke, Scott, McMillan, Malcolm, Melini, Daniele, Mernild, Jacob Sebastian Haugaard, Mohajerani, Yara, Moore, Philip, Mottam, Ruth, Mouginot, Jérémie, Moyano, Gorka, Muir, Alan, Nagler, Thomas, Nield, Grace, Nilsson, Johan, Noel, Brice, Otosaka, Ines, Pattle, Mark E, Peltier, Richard W, Pie, Nadège, Rietbroek, Roelof, Rott, Helmut, Sørensen, Louise Sandberg, Sasgen, Ingo, Save, Himanshu, Scheuchl, Bernd, Schrama, Ernst, Schröder, Ludwig, Seo, Ki-Weon, Simonsen, Sebastian B, Slater, Thomas, Spada, Giorgio, Sutterley, Tyler, Talpe, Matthieu, Tarasov, Lev, Willem, Jan van de Berg, Van Der Wal, Wouter, Van Wessem, Melchior, Vishwakarma, Barmha Dutt, Wiese, David, Wilton, David, Wagner, Thomas, Wouters, Bert, Wuite, Jan
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creator Shepherd, Andrew
Ivins, Erik
Rignot, Eric
Smith, Ben
Van Den Broeke, Michiel
Velicogna, Isabella
Whitehouse, Pippa
Briggs, Kate
Joughin, Ian
Krinner, Gerhard
Nowicki, Sophie
Payne, Tony
Scambos, Ted
Schlegel, Nicole
Geruo, A
Agosta, Cécile
Ahlstrøm, Andreas
Babonis, Greg
Barletta, Valentina
Bjørk, Anders A
Blazquez, Alejandro
Bonin, Jennifer
Colgan, William
Csatho, Beata
Cullather, Richard
Engdahl, Marcus E
Felikson, Denis
Fettweis, Xavier
Forsberg, Rene
Hogg, Anna E
Hubert, Gallee
Gardner, Alex
Gilbert, Lin
Gourmelen, Noel
Groh, Andreas
Gunter, Brian
Hanna, Edward
Harig, Christopher
Helm, Veit
Horvath, Alexander
Horwath, Martin
Khan, Shfaqat
Kjeldsen, Kristian K
Hannes, Konrad
Langen, Peter L
Lecavalier, Benoit
Loomis, Bryant
Luthcke, Scott
McMillan, Malcolm
Melini, Daniele
Mernild, Jacob Sebastian Haugaard
Mohajerani, Yara
Moore, Philip
Mottam, Ruth
Mouginot, Jérémie
Moyano, Gorka
Muir, Alan
Nagler, Thomas
Nield, Grace
Nilsson, Johan
Noel, Brice
Otosaka, Ines
Pattle, Mark E
Peltier, Richard W
Pie, Nadège
Rietbroek, Roelof
Rott, Helmut
Sørensen, Louise Sandberg
Sasgen, Ingo
Save, Himanshu
Scheuchl, Bernd
Schrama, Ernst
Schröder, Ludwig
Seo, Ki-Weon
Simonsen, Sebastian B
Slater, Thomas
Spada, Giorgio
Sutterley, Tyler
Talpe, Matthieu
Tarasov, Lev
Willem, Jan van de Berg
Van Der Wal, Wouter
Van Wessem, Melchior
Vishwakarma, Barmha Dutt
Wiese, David
Wilton, David
Wagner, Thomas
Wouters, Bert
Wuite, Jan
description The Greenland Ice Sheet has been a major contributor to global sea-level rise in recent decades1,2, and it is expected to continue to be so3. Although increases in glacier flow4,5,6 and surface melting7,8,9 have been driven by oceanic10,11,12 and atmospheric13,14 warming, the magnitude and trajectory of the ice sheet’s mass imbalance remain uncertain. Here we compare and combine 26 individual satellite measurements of changes in the ice sheet’s volume, flow and gravitational potential to produce a reconciled estimate of its mass balance. The ice sheet was close to a state of balance in the 1990s, but annual losses have risen since then, peaking at 345 ± 66 billion tonnes per year in 2011. In all, Greenland lost 3,902 ± 342 billion tonnes of ice between 1992 and 2018, causing the mean sea level to rise by 10.8 ± 0.9 millimetres. Using three regional climate models, we show that the reduced surface mass balance has driven 1,964 ± 565 billion tonnes (50.3 per cent) of the ice loss owing to increased meltwater runoff. The remaining 1,938 ± 541 billion tonnes (49.7 per cent) of ice loss was due to increased glacier dynamical imbalance, which rose from 46 ± 37 billion tonnes per year in the 1990s to 87 ± 25 billion tonnes per year since then. The total rate of ice loss slowed to 222 ± 30 billion tonnes per year between 2013 and 2017, on average, as atmospheric circulation favoured cooler conditions15 and ocean temperatures fell at the terminus of Jakobshavn Isbræ16. Cumulative ice losses from Greenland as a whole have been close to the rates predicted by the Intergovernmental Panel on Climate Change for their high-end climate warming scenario17, which forecast an additional 70 to 130 millimetres of global sea-level rise by 2100 compared with their central estimate.
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Although increases in glacier flow4,5,6 and surface melting7,8,9 have been driven by oceanic10,11,12 and atmospheric13,14 warming, the magnitude and trajectory of the ice sheet’s mass imbalance remain uncertain. Here we compare and combine 26 individual satellite measurements of changes in the ice sheet’s volume, flow and gravitational potential to produce a reconciled estimate of its mass balance. The ice sheet was close to a state of balance in the 1990s, but annual losses have risen since then, peaking at 345 ± 66 billion tonnes per year in 2011. In all, Greenland lost 3,902 ± 342 billion tonnes of ice between 1992 and 2018, causing the mean sea level to rise by 10.8 ± 0.9 millimetres. Using three regional climate models, we show that the reduced surface mass balance has driven 1,964 ± 565 billion tonnes (50.3 per cent) of the ice loss owing to increased meltwater runoff. The remaining 1,938 ± 541 billion tonnes (49.7 per cent) of ice loss was due to increased glacier dynamical imbalance, which rose from 46 ± 37 billion tonnes per year in the 1990s to 87 ± 25 billion tonnes per year since then. The total rate of ice loss slowed to 222 ± 30 billion tonnes per year between 2013 and 2017, on average, as atmospheric circulation favoured cooler conditions15 and ocean temperatures fell at the terminus of Jakobshavn Isbræ16. 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W</creatorcontrib><creatorcontrib>Pie, Nadège</creatorcontrib><creatorcontrib>Rietbroek, Roelof</creatorcontrib><creatorcontrib>Rott, Helmut</creatorcontrib><creatorcontrib>Sørensen, Louise Sandberg</creatorcontrib><creatorcontrib>Sasgen, Ingo</creatorcontrib><creatorcontrib>Save, Himanshu</creatorcontrib><creatorcontrib>Scheuchl, Bernd</creatorcontrib><creatorcontrib>Schrama, Ernst</creatorcontrib><creatorcontrib>Schröder, Ludwig</creatorcontrib><creatorcontrib>Seo, Ki-Weon</creatorcontrib><creatorcontrib>Simonsen, Sebastian B</creatorcontrib><creatorcontrib>Slater, Thomas</creatorcontrib><creatorcontrib>Spada, Giorgio</creatorcontrib><creatorcontrib>Sutterley, Tyler</creatorcontrib><creatorcontrib>Talpe, Matthieu</creatorcontrib><creatorcontrib>Tarasov, Lev</creatorcontrib><creatorcontrib>Willem, Jan van de Berg</creatorcontrib><creatorcontrib>Van Der Wal, Wouter</creatorcontrib><creatorcontrib>Van Wessem, Melchior</creatorcontrib><creatorcontrib>Vishwakarma, Barmha Dutt</creatorcontrib><creatorcontrib>Wiese, David</creatorcontrib><creatorcontrib>Wilton, David</creatorcontrib><creatorcontrib>Wagner, Thomas</creatorcontrib><creatorcontrib>Wouters, Bert</creatorcontrib><creatorcontrib>Wuite, Jan</creatorcontrib><title>Mass balance of the Greenland Ice Sheet from 1992 to 2018</title><description>The Greenland Ice Sheet has been a major contributor to global sea-level rise in recent decades1,2, and it is expected to continue to be so3. Although increases in glacier flow4,5,6 and surface melting7,8,9 have been driven by oceanic10,11,12 and atmospheric13,14 warming, the magnitude and trajectory of the ice sheet’s mass imbalance remain uncertain. Here we compare and combine 26 individual satellite measurements of changes in the ice sheet’s volume, flow and gravitational potential to produce a reconciled estimate of its mass balance. The ice sheet was close to a state of balance in the 1990s, but annual losses have risen since then, peaking at 345 ± 66 billion tonnes per year in 2011. In all, Greenland lost 3,902 ± 342 billion tonnes of ice between 1992 and 2018, causing the mean sea level to rise by 10.8 ± 0.9 millimetres. Using three regional climate models, we show that the reduced surface mass balance has driven 1,964 ± 565 billion tonnes (50.3 per cent) of the ice loss owing to increased meltwater runoff. The remaining 1,938 ± 541 billion tonnes (49.7 per cent) of ice loss was due to increased glacier dynamical imbalance, which rose from 46 ± 37 billion tonnes per year in the 1990s to 87 ± 25 billion tonnes per year since then. The total rate of ice loss slowed to 222 ± 30 billion tonnes per year between 2013 and 2017, on average, as atmospheric circulation favoured cooler conditions15 and ocean temperatures fell at the terminus of Jakobshavn Isbræ16. Cumulative ice losses from Greenland as a whole have been close to the rates predicted by the Intergovernmental Panel on Climate Change for their high-end climate warming scenario17, which forecast an additional 70 to 130 millimetres of global sea-level rise by 2100 compared with their central estimate.</description><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><sourceid>3HK</sourceid><recordid>eNrjZLD0TSwuVkhKzEnMS05VyE9TKMlIVXAvSk3NA4qkKHgCBYMzUlNLFNKK8nMVDC0tjRRK8hWMDAwteBhY0xJzilN5oTQ3g6Kba4izh25yUWZxSWZefF5-UWK8oaGRqUG8kbmppZG5oTExagD6OStP</recordid><startdate>2019</startdate><enddate>2019</enddate><creator>Shepherd, Andrew</creator><creator>Ivins, Erik</creator><creator>Rignot, Eric</creator><creator>Smith, Ben</creator><creator>Van Den Broeke, Michiel</creator><creator>Velicogna, Isabella</creator><creator>Whitehouse, Pippa</creator><creator>Briggs, Kate</creator><creator>Joughin, 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Brice ; Otosaka, Ines ; Pattle, Mark E ; Peltier, Richard W ; Pie, Nadège ; Rietbroek, Roelof ; Rott, Helmut ; Sørensen, Louise Sandberg ; Sasgen, Ingo ; Save, Himanshu ; Scheuchl, Bernd ; Schrama, Ernst ; Schröder, Ludwig ; Seo, Ki-Weon ; Simonsen, Sebastian B ; Slater, Thomas ; Spada, Giorgio ; Sutterley, Tyler ; Talpe, Matthieu ; Tarasov, Lev ; Willem, Jan van de Berg ; Van Der Wal, Wouter ; Van Wessem, Melchior ; Vishwakarma, Barmha Dutt ; Wiese, David ; Wilton, David ; Wagner, Thomas ; Wouters, Bert ; Wuite, Jan</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-cristin_nora_11250_27592713</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><toplevel>online_resources</toplevel><creatorcontrib>Shepherd, Andrew</creatorcontrib><creatorcontrib>Ivins, Erik</creatorcontrib><creatorcontrib>Rignot, Eric</creatorcontrib><creatorcontrib>Smith, Ben</creatorcontrib><creatorcontrib>Van Den Broeke, Michiel</creatorcontrib><creatorcontrib>Velicogna, Isabella</creatorcontrib><creatorcontrib>Whitehouse, Pippa</creatorcontrib><creatorcontrib>Briggs, Kate</creatorcontrib><creatorcontrib>Joughin, Ian</creatorcontrib><creatorcontrib>Krinner, Gerhard</creatorcontrib><creatorcontrib>Nowicki, Sophie</creatorcontrib><creatorcontrib>Payne, Tony</creatorcontrib><creatorcontrib>Scambos, Ted</creatorcontrib><creatorcontrib>Schlegel, Nicole</creatorcontrib><creatorcontrib>Geruo, A</creatorcontrib><creatorcontrib>Agosta, Cécile</creatorcontrib><creatorcontrib>Ahlstrøm, Andreas</creatorcontrib><creatorcontrib>Babonis, Greg</creatorcontrib><creatorcontrib>Barletta, Valentina</creatorcontrib><creatorcontrib>Bjørk, Anders A</creatorcontrib><creatorcontrib>Blazquez, Alejandro</creatorcontrib><creatorcontrib>Bonin, Jennifer</creatorcontrib><creatorcontrib>Colgan, William</creatorcontrib><creatorcontrib>Csatho, Beata</creatorcontrib><creatorcontrib>Cullather, Richard</creatorcontrib><creatorcontrib>Engdahl, Marcus E</creatorcontrib><creatorcontrib>Felikson, Denis</creatorcontrib><creatorcontrib>Fettweis, Xavier</creatorcontrib><creatorcontrib>Forsberg, Rene</creatorcontrib><creatorcontrib>Hogg, Anna E</creatorcontrib><creatorcontrib>Hubert, Gallee</creatorcontrib><creatorcontrib>Gardner, Alex</creatorcontrib><creatorcontrib>Gilbert, Lin</creatorcontrib><creatorcontrib>Gourmelen, Noel</creatorcontrib><creatorcontrib>Groh, Andreas</creatorcontrib><creatorcontrib>Gunter, Brian</creatorcontrib><creatorcontrib>Hanna, Edward</creatorcontrib><creatorcontrib>Harig, Christopher</creatorcontrib><creatorcontrib>Helm, Veit</creatorcontrib><creatorcontrib>Horvath, Alexander</creatorcontrib><creatorcontrib>Horwath, Martin</creatorcontrib><creatorcontrib>Khan, Shfaqat</creatorcontrib><creatorcontrib>Kjeldsen, Kristian K</creatorcontrib><creatorcontrib>Hannes, Konrad</creatorcontrib><creatorcontrib>Langen, Peter L</creatorcontrib><creatorcontrib>Lecavalier, Benoit</creatorcontrib><creatorcontrib>Loomis, Bryant</creatorcontrib><creatorcontrib>Luthcke, Scott</creatorcontrib><creatorcontrib>McMillan, Malcolm</creatorcontrib><creatorcontrib>Melini, Daniele</creatorcontrib><creatorcontrib>Mernild, Jacob Sebastian Haugaard</creatorcontrib><creatorcontrib>Mohajerani, Yara</creatorcontrib><creatorcontrib>Moore, Philip</creatorcontrib><creatorcontrib>Mottam, Ruth</creatorcontrib><creatorcontrib>Mouginot, Jérémie</creatorcontrib><creatorcontrib>Moyano, Gorka</creatorcontrib><creatorcontrib>Muir, Alan</creatorcontrib><creatorcontrib>Nagler, Thomas</creatorcontrib><creatorcontrib>Nield, Grace</creatorcontrib><creatorcontrib>Nilsson, Johan</creatorcontrib><creatorcontrib>Noel, Brice</creatorcontrib><creatorcontrib>Otosaka, Ines</creatorcontrib><creatorcontrib>Pattle, Mark E</creatorcontrib><creatorcontrib>Peltier, Richard W</creatorcontrib><creatorcontrib>Pie, Nadège</creatorcontrib><creatorcontrib>Rietbroek, Roelof</creatorcontrib><creatorcontrib>Rott, Helmut</creatorcontrib><creatorcontrib>Sørensen, Louise Sandberg</creatorcontrib><creatorcontrib>Sasgen, Ingo</creatorcontrib><creatorcontrib>Save, Himanshu</creatorcontrib><creatorcontrib>Scheuchl, Bernd</creatorcontrib><creatorcontrib>Schrama, Ernst</creatorcontrib><creatorcontrib>Schröder, Ludwig</creatorcontrib><creatorcontrib>Seo, Ki-Weon</creatorcontrib><creatorcontrib>Simonsen, Sebastian B</creatorcontrib><creatorcontrib>Slater, Thomas</creatorcontrib><creatorcontrib>Spada, Giorgio</creatorcontrib><creatorcontrib>Sutterley, Tyler</creatorcontrib><creatorcontrib>Talpe, Matthieu</creatorcontrib><creatorcontrib>Tarasov, Lev</creatorcontrib><creatorcontrib>Willem, Jan van de Berg</creatorcontrib><creatorcontrib>Van Der Wal, Wouter</creatorcontrib><creatorcontrib>Van Wessem, Melchior</creatorcontrib><creatorcontrib>Vishwakarma, Barmha Dutt</creatorcontrib><creatorcontrib>Wiese, David</creatorcontrib><creatorcontrib>Wilton, David</creatorcontrib><creatorcontrib>Wagner, Thomas</creatorcontrib><creatorcontrib>Wouters, Bert</creatorcontrib><creatorcontrib>Wuite, Jan</creatorcontrib><collection>NORA - Norwegian Open Research Archives</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Shepherd, Andrew</au><au>Ivins, Erik</au><au>Rignot, Eric</au><au>Smith, Ben</au><au>Van Den Broeke, Michiel</au><au>Velicogna, Isabella</au><au>Whitehouse, Pippa</au><au>Briggs, Kate</au><au>Joughin, Ian</au><au>Krinner, Gerhard</au><au>Nowicki, Sophie</au><au>Payne, Tony</au><au>Scambos, Ted</au><au>Schlegel, Nicole</au><au>Geruo, A</au><au>Agosta, Cécile</au><au>Ahlstrøm, Andreas</au><au>Babonis, Greg</au><au>Barletta, Valentina</au><au>Bjørk, Anders A</au><au>Blazquez, Alejandro</au><au>Bonin, Jennifer</au><au>Colgan, William</au><au>Csatho, Beata</au><au>Cullather, Richard</au><au>Engdahl, Marcus E</au><au>Felikson, Denis</au><au>Fettweis, Xavier</au><au>Forsberg, Rene</au><au>Hogg, Anna E</au><au>Hubert, Gallee</au><au>Gardner, Alex</au><au>Gilbert, Lin</au><au>Gourmelen, Noel</au><au>Groh, Andreas</au><au>Gunter, Brian</au><au>Hanna, Edward</au><au>Harig, Christopher</au><au>Helm, Veit</au><au>Horvath, Alexander</au><au>Horwath, Martin</au><au>Khan, Shfaqat</au><au>Kjeldsen, Kristian K</au><au>Hannes, Konrad</au><au>Langen, Peter L</au><au>Lecavalier, Benoit</au><au>Loomis, Bryant</au><au>Luthcke, Scott</au><au>McMillan, Malcolm</au><au>Melini, Daniele</au><au>Mernild, Jacob Sebastian Haugaard</au><au>Mohajerani, Yara</au><au>Moore, Philip</au><au>Mottam, Ruth</au><au>Mouginot, Jérémie</au><au>Moyano, Gorka</au><au>Muir, Alan</au><au>Nagler, Thomas</au><au>Nield, Grace</au><au>Nilsson, Johan</au><au>Noel, Brice</au><au>Otosaka, Ines</au><au>Pattle, Mark E</au><au>Peltier, Richard W</au><au>Pie, Nadège</au><au>Rietbroek, Roelof</au><au>Rott, Helmut</au><au>Sørensen, Louise Sandberg</au><au>Sasgen, Ingo</au><au>Save, Himanshu</au><au>Scheuchl, Bernd</au><au>Schrama, Ernst</au><au>Schröder, Ludwig</au><au>Seo, Ki-Weon</au><au>Simonsen, Sebastian B</au><au>Slater, Thomas</au><au>Spada, Giorgio</au><au>Sutterley, Tyler</au><au>Talpe, Matthieu</au><au>Tarasov, Lev</au><au>Willem, Jan van de Berg</au><au>Van Der Wal, Wouter</au><au>Van Wessem, Melchior</au><au>Vishwakarma, Barmha Dutt</au><au>Wiese, David</au><au>Wilton, David</au><au>Wagner, Thomas</au><au>Wouters, Bert</au><au>Wuite, Jan</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mass balance of the Greenland Ice Sheet from 1992 to 2018</atitle><date>2019</date><risdate>2019</risdate><abstract>The Greenland Ice Sheet has been a major contributor to global sea-level rise in recent decades1,2, and it is expected to continue to be so3. Although increases in glacier flow4,5,6 and surface melting7,8,9 have been driven by oceanic10,11,12 and atmospheric13,14 warming, the magnitude and trajectory of the ice sheet’s mass imbalance remain uncertain. Here we compare and combine 26 individual satellite measurements of changes in the ice sheet’s volume, flow and gravitational potential to produce a reconciled estimate of its mass balance. The ice sheet was close to a state of balance in the 1990s, but annual losses have risen since then, peaking at 345 ± 66 billion tonnes per year in 2011. In all, Greenland lost 3,902 ± 342 billion tonnes of ice between 1992 and 2018, causing the mean sea level to rise by 10.8 ± 0.9 millimetres. Using three regional climate models, we show that the reduced surface mass balance has driven 1,964 ± 565 billion tonnes (50.3 per cent) of the ice loss owing to increased meltwater runoff. The remaining 1,938 ± 541 billion tonnes (49.7 per cent) of ice loss was due to increased glacier dynamical imbalance, which rose from 46 ± 37 billion tonnes per year in the 1990s to 87 ± 25 billion tonnes per year since then. The total rate of ice loss slowed to 222 ± 30 billion tonnes per year between 2013 and 2017, on average, as atmospheric circulation favoured cooler conditions15 and ocean temperatures fell at the terminus of Jakobshavn Isbræ16. Cumulative ice losses from Greenland as a whole have been close to the rates predicted by the Intergovernmental Panel on Climate Change for their high-end climate warming scenario17, which forecast an additional 70 to 130 millimetres of global sea-level rise by 2100 compared with their central estimate.</abstract><pub>Nature Research</pub><oa>free_for_read</oa></addata></record>
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title Mass balance of the Greenland Ice Sheet from 1992 to 2018
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