Rapid ablation zone expansion amplifies north Greenland mass loss: modelled (RACMO2) and observed (MODIS) data sets

Since the early 1990s, the Greenland ice sheet (GrIS) has been losing mass at an accelerating rate, primarily due to enhanced meltwater runoff following an atmospheric warming of ~1ºC. Here we show that a pronounced latitudinal contrast exists in the GrIS response to recent warming. The ablation are...

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Main Author: Noël, Brice P Y
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.904428
https://doi.org/10.1594/PANGAEA.904428
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.904428
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.904428 2023-05-15T13:12:05+02:00 Rapid ablation zone expansion amplifies north Greenland mass loss: modelled (RACMO2) and observed (MODIS) data sets Noël, Brice P Y LATITUDE: 73.000000 * LONGITUDE: -42.000000 2019-08-02 text/tab-separated-values, 36 data points https://doi.pangaea.de/10.1594/PANGAEA.904428 https://doi.org/10.1594/PANGAEA.904428 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.904428 https://doi.org/10.1594/PANGAEA.904428 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY File format File name File size Greenland Greenland_Ice RACMO Uniform resource locator/link to file Dataset 2019 ftpangaea https://doi.org/10.1594/PANGAEA.904428 2023-01-20T09:12:36Z Since the early 1990s, the Greenland ice sheet (GrIS) has been losing mass at an accelerating rate, primarily due to enhanced meltwater runoff following an atmospheric warming of ~1ºC. Here we show that a pronounced latitudinal contrast exists in the GrIS response to recent warming. The ablation area in north Greenland expanded by 46%, almost twice as much as in the south (+25%), significantly increasing the relative contribution of the north to total GrIS mass loss. This latitudinal contrast originates from a different response to the recent change in large-scale Arctic summertime atmospheric circulation, promoting southwesterly advection of warm air towards the GrIS. In the southwest, persistent high atmospheric pressure reduced cloudiness, increasing runoff through enhanced absorption of solar radiation; in contrast, increased early-summer cloudiness in north Greenland enhanced atmospheric warming through decreased longwave heat loss. This triggered a rapid snowline retreat, causing early bare ice exposure, amplifying northern runoff. The data set includes: 5.5 km data: annual mean summertime (June-July-August) shortwave down/upward radiation (swsd/swsu; W m-2), longwave down/upward radiation (lwsd/lwsu; W m-2), surface albedo (alb; unitless) and cloud content (qci; kg m-2) modelled by RACMO2.3p2 at 5.5 km spatial resolution for the period 1958-2017. 1 km data: annual cumulative meltwater runoff (kg m-2 or mm w.e.) modelled by RACMO2.3p2 at 5.5 km resolution and further statistically downscaled to 1 km for the period 1958-2017. Annual maximum bare ice extent (unitless) remotely sensed by MODIS at 1 km spatial resolution for the period 2000-2018. Mask file at 1 km resolution including longitude/latitude coordinates and outlines of the seven Greenland ice sheet sectors investigated in the study. Additional RACMO2.3p2 data, including daily downscaled surface mass balance (SMB) components at 1 km and modelled climate variables at 5.5 km resolution, are freely available from the authors upon request and without ... Dataset albedo Arctic Greenland Ice Sheet North Greenland PANGAEA - Data Publisher for Earth & Environmental Science Arctic Greenland ENVELOPE(-42.000000,-42.000000,73.000000,73.000000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic File format
File name
File size
Greenland
Greenland_Ice
RACMO
Uniform resource locator/link to file
spellingShingle File format
File name
File size
Greenland
Greenland_Ice
RACMO
Uniform resource locator/link to file
Noël, Brice P Y
Rapid ablation zone expansion amplifies north Greenland mass loss: modelled (RACMO2) and observed (MODIS) data sets
topic_facet File format
File name
File size
Greenland
Greenland_Ice
RACMO
Uniform resource locator/link to file
description Since the early 1990s, the Greenland ice sheet (GrIS) has been losing mass at an accelerating rate, primarily due to enhanced meltwater runoff following an atmospheric warming of ~1ºC. Here we show that a pronounced latitudinal contrast exists in the GrIS response to recent warming. The ablation area in north Greenland expanded by 46%, almost twice as much as in the south (+25%), significantly increasing the relative contribution of the north to total GrIS mass loss. This latitudinal contrast originates from a different response to the recent change in large-scale Arctic summertime atmospheric circulation, promoting southwesterly advection of warm air towards the GrIS. In the southwest, persistent high atmospheric pressure reduced cloudiness, increasing runoff through enhanced absorption of solar radiation; in contrast, increased early-summer cloudiness in north Greenland enhanced atmospheric warming through decreased longwave heat loss. This triggered a rapid snowline retreat, causing early bare ice exposure, amplifying northern runoff. The data set includes: 5.5 km data: annual mean summertime (June-July-August) shortwave down/upward radiation (swsd/swsu; W m-2), longwave down/upward radiation (lwsd/lwsu; W m-2), surface albedo (alb; unitless) and cloud content (qci; kg m-2) modelled by RACMO2.3p2 at 5.5 km spatial resolution for the period 1958-2017. 1 km data: annual cumulative meltwater runoff (kg m-2 or mm w.e.) modelled by RACMO2.3p2 at 5.5 km resolution and further statistically downscaled to 1 km for the period 1958-2017. Annual maximum bare ice extent (unitless) remotely sensed by MODIS at 1 km spatial resolution for the period 2000-2018. Mask file at 1 km resolution including longitude/latitude coordinates and outlines of the seven Greenland ice sheet sectors investigated in the study. Additional RACMO2.3p2 data, including daily downscaled surface mass balance (SMB) components at 1 km and modelled climate variables at 5.5 km resolution, are freely available from the authors upon request and without ...
format Dataset
author Noël, Brice P Y
author_facet Noël, Brice P Y
author_sort Noël, Brice P Y
title Rapid ablation zone expansion amplifies north Greenland mass loss: modelled (RACMO2) and observed (MODIS) data sets
title_short Rapid ablation zone expansion amplifies north Greenland mass loss: modelled (RACMO2) and observed (MODIS) data sets
title_full Rapid ablation zone expansion amplifies north Greenland mass loss: modelled (RACMO2) and observed (MODIS) data sets
title_fullStr Rapid ablation zone expansion amplifies north Greenland mass loss: modelled (RACMO2) and observed (MODIS) data sets
title_full_unstemmed Rapid ablation zone expansion amplifies north Greenland mass loss: modelled (RACMO2) and observed (MODIS) data sets
title_sort rapid ablation zone expansion amplifies north greenland mass loss: modelled (racmo2) and observed (modis) data sets
publisher PANGAEA
publishDate 2019
url https://doi.pangaea.de/10.1594/PANGAEA.904428
https://doi.org/10.1594/PANGAEA.904428
op_coverage LATITUDE: 73.000000 * LONGITUDE: -42.000000
long_lat ENVELOPE(-42.000000,-42.000000,73.000000,73.000000)
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre albedo
Arctic
Greenland
Ice Sheet
North Greenland
genre_facet albedo
Arctic
Greenland
Ice Sheet
North Greenland
op_relation https://doi.pangaea.de/10.1594/PANGAEA.904428
https://doi.org/10.1594/PANGAEA.904428
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.904428
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