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Mass balance of the Greenland and Antarctic ice sheets from 1992 to 2020

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Mass balance of the Greenland and Antarctic ice sheets from 1992 to 2020. / The IMBIE Team.
In: Earth System Science Data, Vol. 15, No. 4, 20.04.2023, p. 1597-1616.

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The IMBIE Team 2023, 'Mass balance of the Greenland and Antarctic ice sheets from 1992 to 2020', Earth System Science Data, vol. 15, no. 4, pp. 1597-1616. https://doi.org/10.5194/essd-15-1597-2023

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The IMBIE Team. Mass balance of the Greenland and Antarctic ice sheets from 1992 to 2020. Earth System Science Data. 2023 Apr 20;15(4):1597-1616. doi: 10.5194/essd-15-1597-2023

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The IMBIE Team. / Mass balance of the Greenland and Antarctic ice sheets from 1992 to 2020. In: Earth System Science Data. 2023 ; Vol. 15, No. 4. pp. 1597-1616.

Bibtex

@article{28e1a6435cee46978c8d26f996db50c3,
title = "Mass balance of the Greenland and Antarctic ice sheets from 1992 to 2020",
abstract = "Ice losses from the Greenland and Antarctic ice sheets have accelerated since the 1990s, accounting for a significant increase in the global mean sea level. Here, we present a new 29-year record of ice sheet mass balance from 1992 to 2020 from the Ice Sheet Mass Balance Inter-comparison Exercise (IMBIE). We compare and combine 50 independent estimates of ice sheet mass balance derived from satellite observations of temporal changes in ice sheet flow, in ice sheet volume, and in Earth's gravity field. Between 1992 and 2020, the ice sheets contributed 21.0±1.9 mm to global mean sea level, with the rate of mass loss rising from 105 Gt yr−1 between 1992 and 1996 to 372 Gt yr−1 between 2016 and 2020. In Greenland, the rate of mass loss is 169±9 Gt yr−1 between 1992 and 2020, but there are large inter-annual variations in mass balance, with mass loss ranging from 86 Gt yr−1 in 2017 to 444 Gt yr−1 in 2019 due to large variability in surface mass balance. In Antarctica, ice losses continue to be dominated by mass loss from West Antarctica (82±9 Gt yr−1) and, to a lesser extent, from the Antarctic Peninsula (13±5 Gt yr−1). East Antarctica remains close to a state of balance, with a small gain of 3±15 Gt yr−1, but is the most uncertain component of Antarctica's mass balance. The dataset is publicly available at https://doi.org/10.5285/77B64C55-7166-4A06-9DEF-2E400398E452 (IMBIE Team, 2021).",
keywords = "General Earth and Planetary Sciences",
author = "{The IMBIE Team} and Otosaka, {In{\`e}s N.} and Andrew Shepherd and Ivins, {Erik R.} and Nicole-Jeanne Schlegel and Charles Amory and {van den Broeke}, {Michiel R.} and Martin Horwath and Ian Joughin and King, {Michalea D.} and Gerhard Krinner and Sophie Nowicki and Payne, {Anthony J.} and Eric Rignot and Ted Scambos and Simon, {Karen M.} and Smith, {Benjamin E.} and S{\o}rensen, {Louise S.} and Isabella Velicogna and Whitehouse, {Pippa L.} and Geruo A and C{\'e}cile Agosta and Ahlstr{\o}m, {Andreas P.} and Alejandro Blazquez and William Colgan and Engdahl, {Marcus E.} and Xavier Fettweis and Rene Forsberg and Hubert Gall{\'e}e and Alex Gardner and Lin Gilbert and Noel Gourmelen and Andreas Groh and Gunter, {Brian C.} and Christopher Harig and Veit Helm and Khan, {Shfaqat Abbas} and Christoph Kittel and Hannes Konrad and Langen, {Peter L.} and Lecavalier, {Benoit S.} and Chia-Chun Liang and Loomis, {Bryant D.} and Malcolm McMillan and Daniele Melini and Mernild, {Sebastian H.} and Ruth Mottram and Jeremie Mouginot and Johan Nilsson and Brice No{\"e}l and Pattle, {Mark E.}",
year = "2023",
month = apr,
day = "20",
doi = "10.5194/essd-15-1597-2023",
language = "English",
volume = "15",
pages = "1597--1616",
journal = "Earth System Science Data",
issn = "1866-3508",
publisher = "Copernicus Publications",
number = "4",

}

RIS

TY - JOUR

T1 - Mass balance of the Greenland and Antarctic ice sheets from 1992 to 2020

AU - The IMBIE Team

AU - Otosaka, Inès N.

AU - Shepherd, Andrew

AU - Ivins, Erik R.

AU - Schlegel, Nicole-Jeanne

AU - Amory, Charles

AU - van den Broeke, Michiel R.

AU - Horwath, Martin

AU - Joughin, Ian

AU - King, Michalea D.

AU - Krinner, Gerhard

AU - Nowicki, Sophie

AU - Payne, Anthony J.

AU - Rignot, Eric

AU - Scambos, Ted

AU - Simon, Karen M.

AU - Smith, Benjamin E.

AU - Sørensen, Louise S.

AU - Velicogna, Isabella

AU - Whitehouse, Pippa L.

AU - A, Geruo

AU - Agosta, Cécile

AU - Ahlstrøm, Andreas P.

AU - Blazquez, Alejandro

AU - Colgan, William

AU - Engdahl, Marcus E.

AU - Fettweis, Xavier

AU - Forsberg, Rene

AU - Gallée, Hubert

AU - Gardner, Alex

AU - Gilbert, Lin

AU - Gourmelen, Noel

AU - Groh, Andreas

AU - Gunter, Brian C.

AU - Harig, Christopher

AU - Helm, Veit

AU - Khan, Shfaqat Abbas

AU - Kittel, Christoph

AU - Konrad, Hannes

AU - Langen, Peter L.

AU - Lecavalier, Benoit S.

AU - Liang, Chia-Chun

AU - Loomis, Bryant D.

AU - McMillan, Malcolm

AU - Melini, Daniele

AU - Mernild, Sebastian H.

AU - Mottram, Ruth

AU - Mouginot, Jeremie

AU - Nilsson, Johan

AU - Noël, Brice

AU - Pattle, Mark E.

PY - 2023/4/20

Y1 - 2023/4/20

N2 - Ice losses from the Greenland and Antarctic ice sheets have accelerated since the 1990s, accounting for a significant increase in the global mean sea level. Here, we present a new 29-year record of ice sheet mass balance from 1992 to 2020 from the Ice Sheet Mass Balance Inter-comparison Exercise (IMBIE). We compare and combine 50 independent estimates of ice sheet mass balance derived from satellite observations of temporal changes in ice sheet flow, in ice sheet volume, and in Earth's gravity field. Between 1992 and 2020, the ice sheets contributed 21.0±1.9 mm to global mean sea level, with the rate of mass loss rising from 105 Gt yr−1 between 1992 and 1996 to 372 Gt yr−1 between 2016 and 2020. In Greenland, the rate of mass loss is 169±9 Gt yr−1 between 1992 and 2020, but there are large inter-annual variations in mass balance, with mass loss ranging from 86 Gt yr−1 in 2017 to 444 Gt yr−1 in 2019 due to large variability in surface mass balance. In Antarctica, ice losses continue to be dominated by mass loss from West Antarctica (82±9 Gt yr−1) and, to a lesser extent, from the Antarctic Peninsula (13±5 Gt yr−1). East Antarctica remains close to a state of balance, with a small gain of 3±15 Gt yr−1, but is the most uncertain component of Antarctica's mass balance. The dataset is publicly available at https://doi.org/10.5285/77B64C55-7166-4A06-9DEF-2E400398E452 (IMBIE Team, 2021).

AB - Ice losses from the Greenland and Antarctic ice sheets have accelerated since the 1990s, accounting for a significant increase in the global mean sea level. Here, we present a new 29-year record of ice sheet mass balance from 1992 to 2020 from the Ice Sheet Mass Balance Inter-comparison Exercise (IMBIE). We compare and combine 50 independent estimates of ice sheet mass balance derived from satellite observations of temporal changes in ice sheet flow, in ice sheet volume, and in Earth's gravity field. Between 1992 and 2020, the ice sheets contributed 21.0±1.9 mm to global mean sea level, with the rate of mass loss rising from 105 Gt yr−1 between 1992 and 1996 to 372 Gt yr−1 between 2016 and 2020. In Greenland, the rate of mass loss is 169±9 Gt yr−1 between 1992 and 2020, but there are large inter-annual variations in mass balance, with mass loss ranging from 86 Gt yr−1 in 2017 to 444 Gt yr−1 in 2019 due to large variability in surface mass balance. In Antarctica, ice losses continue to be dominated by mass loss from West Antarctica (82±9 Gt yr−1) and, to a lesser extent, from the Antarctic Peninsula (13±5 Gt yr−1). East Antarctica remains close to a state of balance, with a small gain of 3±15 Gt yr−1, but is the most uncertain component of Antarctica's mass balance. The dataset is publicly available at https://doi.org/10.5285/77B64C55-7166-4A06-9DEF-2E400398E452 (IMBIE Team, 2021).

KW - General Earth and Planetary Sciences

U2 - 10.5194/essd-15-1597-2023

DO - 10.5194/essd-15-1597-2023

M3 - Journal article

VL - 15

SP - 1597

EP - 1616

JO - Earth System Science Data

JF - Earth System Science Data

SN - 1866-3508

IS - 4

ER -