author_facet Cullather, Richard I.
Andrews, Lauren C.
Croteau, Michael J.
Digirolamo, Nicolo E.
Hall, Dorothy K.
Lim, Young‐Kwon
Loomis, Bryant D.
Shuman, Christopher A.
Nowicki, Sophie M. J.
Cullather, Richard I.
Andrews, Lauren C.
Croteau, Michael J.
Digirolamo, Nicolo E.
Hall, Dorothy K.
Lim, Young‐Kwon
Loomis, Bryant D.
Shuman, Christopher A.
Nowicki, Sophie M. J.
author Cullather, Richard I.
Andrews, Lauren C.
Croteau, Michael J.
Digirolamo, Nicolo E.
Hall, Dorothy K.
Lim, Young‐Kwon
Loomis, Bryant D.
Shuman, Christopher A.
Nowicki, Sophie M. J.
spellingShingle Cullather, Richard I.
Andrews, Lauren C.
Croteau, Michael J.
Digirolamo, Nicolo E.
Hall, Dorothy K.
Lim, Young‐Kwon
Loomis, Bryant D.
Shuman, Christopher A.
Nowicki, Sophie M. J.
Geophysical Research Letters
Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
General Earth and Planetary Sciences
Geophysics
author_sort cullather, richard i.
spelling Cullather, Richard I. Andrews, Lauren C. Croteau, Michael J. Digirolamo, Nicolo E. Hall, Dorothy K. Lim, Young‐Kwon Loomis, Bryant D. Shuman, Christopher A. Nowicki, Sophie M. J. 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2020gl087263 <jats:title>Abstract</jats:title><jats:p>Current mass loss on the Greenland Ice Sheet (GrIS) includes a significant contribution from surface runoff. The circumstances associated with melt events are important for understanding the global sea level contribution of the GrIS. In late July 2019, surface melt occurred over 62% of the GrIS, including Summit Station. The general circulation leading to the event is found to be dissimilar to 2012 and other events documented in the 21st century, with warm air associated with remote atmospheric blocking over western Europe eventually transiting west to the GrIS. Gravimetric data indicate that the 2019 summer mass loss was 137 Gt more than the 2004–2010 median, or about 92% of the 2012 record. Mass loss during the event was significant in GrIS northeastern regions in 2019. As compared to 2012, the southwest did not fully participate. Similar circulation patterns have not previously been associated with significant melt.</jats:p> Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet Geophysical Research Letters
doi_str_mv 10.1029/2020gl087263
facet_avail Online
Free
finc_class_facet Geologie und Paläontologie
Geographie
Physik
format ElectronicArticle
fullrecord blob:ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDIwZ2wwODcyNjM
id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDIwZ2wwODcyNjM
institution DE-L229
DE-D275
DE-Bn3
DE-Brt1
DE-Zwi2
DE-D161
DE-Gla1
DE-Zi4
DE-15
DE-Pl11
DE-Rs1
DE-105
DE-14
DE-Ch1
imprint American Geophysical Union (AGU), 2020
imprint_str_mv American Geophysical Union (AGU), 2020
issn 0094-8276
1944-8007
issn_str_mv 0094-8276
1944-8007
language English
mega_collection American Geophysical Union (AGU) (CrossRef)
match_str cullather2020anomalouscirculationinjuly2019resultinginmasslossonthegreenlandicesheet
publishDateSort 2020
publisher American Geophysical Union (AGU)
recordtype ai
record_format ai
series Geophysical Research Letters
source_id 49
title Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_unstemmed Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_full Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_fullStr Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_full_unstemmed Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_short Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_sort anomalous circulation in july 2019 resulting in mass loss on the greenland ice sheet
topic General Earth and Planetary Sciences
Geophysics
url http://dx.doi.org/10.1029/2020gl087263
publishDate 2020
physical
description <jats:title>Abstract</jats:title><jats:p>Current mass loss on the Greenland Ice Sheet (GrIS) includes a significant contribution from surface runoff. The circumstances associated with melt events are important for understanding the global sea level contribution of the GrIS. In late July 2019, surface melt occurred over 62% of the GrIS, including Summit Station. The general circulation leading to the event is found to be dissimilar to 2012 and other events documented in the 21st century, with warm air associated with remote atmospheric blocking over western Europe eventually transiting west to the GrIS. Gravimetric data indicate that the 2019 summer mass loss was 137 Gt more than the 2004–2010 median, or about 92% of the 2012 record. Mass loss during the event was significant in GrIS northeastern regions in 2019. As compared to 2012, the southwest did not fully participate. Similar circulation patterns have not previously been associated with significant melt.</jats:p>
container_issue 17
container_start_page 0
container_title Geophysical Research Letters
container_volume 47
format_de105 Article, E-Article
format_de14 Article, E-Article
format_de15 Article, E-Article
format_de520 Article, E-Article
format_de540 Article, E-Article
format_dech1 Article, E-Article
format_ded117 Article, E-Article
format_degla1 E-Article
format_del152 Buch
format_del189 Article, E-Article
format_dezi4 Article
format_dezwi2 Article, E-Article
format_finc Article, E-Article
format_nrw Article, E-Article
_version_ 1792344056153505808
geogr_code not assigned
last_indexed 2024-03-01T17:01:27.699Z
geogr_code_person not assigned
openURL url_ver=Z39.88-2004&ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fvufind.svn.sourceforge.net%3Agenerator&rft.title=Anomalous+Circulation+in+July+2019+Resulting+in+Mass+Loss+on+the+Greenland+Ice+Sheet&rft.date=2020-09-16&genre=article&issn=1944-8007&volume=47&issue=17&jtitle=Geophysical+Research+Letters&atitle=Anomalous+Circulation+in+July+2019+Resulting+in+Mass+Loss+on+the+Greenland+Ice+Sheet&aulast=Nowicki&aufirst=Sophie+M.+J.&rft_id=info%3Adoi%2F10.1029%2F2020gl087263&rft.language%5B0%5D=eng
SOLR
_version_ 1792344056153505808
author Cullather, Richard I., Andrews, Lauren C., Croteau, Michael J., Digirolamo, Nicolo E., Hall, Dorothy K., Lim, Young‐Kwon, Loomis, Bryant D., Shuman, Christopher A., Nowicki, Sophie M. J.
author_facet Cullather, Richard I., Andrews, Lauren C., Croteau, Michael J., Digirolamo, Nicolo E., Hall, Dorothy K., Lim, Young‐Kwon, Loomis, Bryant D., Shuman, Christopher A., Nowicki, Sophie M. J., Cullather, Richard I., Andrews, Lauren C., Croteau, Michael J., Digirolamo, Nicolo E., Hall, Dorothy K., Lim, Young‐Kwon, Loomis, Bryant D., Shuman, Christopher A., Nowicki, Sophie M. J.
author_sort cullather, richard i.
container_issue 17
container_start_page 0
container_title Geophysical Research Letters
container_volume 47
description <jats:title>Abstract</jats:title><jats:p>Current mass loss on the Greenland Ice Sheet (GrIS) includes a significant contribution from surface runoff. The circumstances associated with melt events are important for understanding the global sea level contribution of the GrIS. In late July 2019, surface melt occurred over 62% of the GrIS, including Summit Station. The general circulation leading to the event is found to be dissimilar to 2012 and other events documented in the 21st century, with warm air associated with remote atmospheric blocking over western Europe eventually transiting west to the GrIS. Gravimetric data indicate that the 2019 summer mass loss was 137 Gt more than the 2004–2010 median, or about 92% of the 2012 record. Mass loss during the event was significant in GrIS northeastern regions in 2019. As compared to 2012, the southwest did not fully participate. Similar circulation patterns have not previously been associated with significant melt.</jats:p>
doi_str_mv 10.1029/2020gl087263
facet_avail Online, Free
finc_class_facet Geologie und Paläontologie, Geographie, Physik
format ElectronicArticle
format_de105 Article, E-Article
format_de14 Article, E-Article
format_de15 Article, E-Article
format_de520 Article, E-Article
format_de540 Article, E-Article
format_dech1 Article, E-Article
format_ded117 Article, E-Article
format_degla1 E-Article
format_del152 Buch
format_del189 Article, E-Article
format_dezi4 Article
format_dezwi2 Article, E-Article
format_finc Article, E-Article
format_nrw Article, E-Article
geogr_code not assigned
geogr_code_person not assigned
id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDIwZ2wwODcyNjM
imprint American Geophysical Union (AGU), 2020
imprint_str_mv American Geophysical Union (AGU), 2020
institution DE-L229, DE-D275, DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161, DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1
issn 0094-8276, 1944-8007
issn_str_mv 0094-8276, 1944-8007
language English
last_indexed 2024-03-01T17:01:27.699Z
match_str cullather2020anomalouscirculationinjuly2019resultinginmasslossonthegreenlandicesheet
mega_collection American Geophysical Union (AGU) (CrossRef)
physical
publishDate 2020
publishDateSort 2020
publisher American Geophysical Union (AGU)
record_format ai
recordtype ai
series Geophysical Research Letters
source_id 49
spelling Cullather, Richard I. Andrews, Lauren C. Croteau, Michael J. Digirolamo, Nicolo E. Hall, Dorothy K. Lim, Young‐Kwon Loomis, Bryant D. Shuman, Christopher A. Nowicki, Sophie M. J. 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2020gl087263 <jats:title>Abstract</jats:title><jats:p>Current mass loss on the Greenland Ice Sheet (GrIS) includes a significant contribution from surface runoff. The circumstances associated with melt events are important for understanding the global sea level contribution of the GrIS. In late July 2019, surface melt occurred over 62% of the GrIS, including Summit Station. The general circulation leading to the event is found to be dissimilar to 2012 and other events documented in the 21st century, with warm air associated with remote atmospheric blocking over western Europe eventually transiting west to the GrIS. Gravimetric data indicate that the 2019 summer mass loss was 137 Gt more than the 2004–2010 median, or about 92% of the 2012 record. Mass loss during the event was significant in GrIS northeastern regions in 2019. As compared to 2012, the southwest did not fully participate. Similar circulation patterns have not previously been associated with significant melt.</jats:p> Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet Geophysical Research Letters
spellingShingle Cullather, Richard I., Andrews, Lauren C., Croteau, Michael J., Digirolamo, Nicolo E., Hall, Dorothy K., Lim, Young‐Kwon, Loomis, Bryant D., Shuman, Christopher A., Nowicki, Sophie M. J., Geophysical Research Letters, Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet, General Earth and Planetary Sciences, Geophysics
title Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_full Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_fullStr Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_full_unstemmed Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_short Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
title_sort anomalous circulation in july 2019 resulting in mass loss on the greenland ice sheet
title_unstemmed Anomalous Circulation in July 2019 Resulting in Mass Loss on the Greenland Ice Sheet
topic General Earth and Planetary Sciences, Geophysics
url http://dx.doi.org/10.1029/2020gl087263