The footprints of 16 year trends of Arctic springtime cloud and radiation properties on September sea ice retreat
The most prominent September Arctic sea ice decline over the period of 2000-2015 occurs over the Siberian Sea, Laptev Sea, and Kara Sea. The satellite observed and retrieved sea ice concentration (SIC) and cloud/radiation properties over the Arctic (70 degrees-90 degrees N) have been used to investi...
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Online Access: | http://hdl.handle.net/10150/623224 https://doi.org/10.1002/2016JD026020 |
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ftunivarizona:oai:repository.arizona.edu:10150/623224 2023-05-15T14:25:05+02:00 The footprints of 16 year trends of Arctic springtime cloud and radiation properties on September sea ice retreat Huang, Yiyi Dong, Xiquan Xi, Baike Dolinar, Erica K. Stanfield, Ryan E. Univ Arizona, Dept Hydrol & Atmospher Sci Department of Hydrology & Atmospheric Sciences; University of Arizona; Tucson Arizona USA Department of Atmospheric Sciences; University of North Dakota; Grand Forks North Dakota USA 2017-02-27 http://hdl.handle.net/10150/623224 https://doi.org/10.1002/2016JD026020 en eng AMER GEOPHYSICAL UNION http://doi.wiley.com/10.1002/2016JD026020 The footprints of 16 year trends of Arctic springtime cloud and radiation properties on September sea ice retreat 2017, 122 (4):2179 Journal of Geophysical Research: Atmospheres 2169897X doi:10.1002/2016JD026020 http://hdl.handle.net/10150/623224 Journal of Geophysical Research: Atmospheres ©2017. American Geophysical Union. All Rights Reserved. Article 2017 ftunivarizona https://doi.org/10.1002/2016JD026020 2020-06-14T08:15:20Z The most prominent September Arctic sea ice decline over the period of 2000-2015 occurs over the Siberian Sea, Laptev Sea, and Kara Sea. The satellite observed and retrieved sea ice concentration (SIC) and cloud/radiation properties over the Arctic (70 degrees-90 degrees N) have been used to investigate the impact of springtime cloud and radiation properties on September SIC variation. Positive trends of cloud fractions, cloud water paths, and surface downward longwave flux at the surface over the September sea ice retreat areas are found over the period of 1 March to 14 May, while negative trends are found over the period of 15 May to 28 June. The spatial distributions of correlations between springtime cloud/radiation properties and September SIC have been calculated, indicating that increasing cloud fractions and downward longwave flux during springtime tend to enhance sea ice melting due to strong cloud warming effect. Surface downward and upward shortwave fluxes play an important role from May to June when the onset of sea ice melting occurs. The comparison between linearly detrended and nondetrended of each parameter indicates that significant impact of cloud and radiation properties on September sea ice retreat occurs over the Chukchi/Beaufort Sea at interannual time scale, especially over the period of 31 March to 29 April, while strongest climatological trends are found over the Laptev/Siberian Sea. NOAA MAPP under grant at the University of North Dakota [NA13OAR4310105]; NASA CERES project under grant at the University of Arizona [NNX17AC52G] 6 month embargo; First published: 21 February 2017 This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. Article in Journal/Newspaper Arctic Arctic Beaufort Sea Chukchi Kara Sea laptev Laptev Sea Sea ice The University of Arizona: UA Campus Repository Arctic Kara Sea Laptev Sea Journal of Geophysical Research: Atmospheres 122 4 2179 2193 |
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Open Polar |
collection |
The University of Arizona: UA Campus Repository |
op_collection_id |
ftunivarizona |
language |
English |
description |
The most prominent September Arctic sea ice decline over the period of 2000-2015 occurs over the Siberian Sea, Laptev Sea, and Kara Sea. The satellite observed and retrieved sea ice concentration (SIC) and cloud/radiation properties over the Arctic (70 degrees-90 degrees N) have been used to investigate the impact of springtime cloud and radiation properties on September SIC variation. Positive trends of cloud fractions, cloud water paths, and surface downward longwave flux at the surface over the September sea ice retreat areas are found over the period of 1 March to 14 May, while negative trends are found over the period of 15 May to 28 June. The spatial distributions of correlations between springtime cloud/radiation properties and September SIC have been calculated, indicating that increasing cloud fractions and downward longwave flux during springtime tend to enhance sea ice melting due to strong cloud warming effect. Surface downward and upward shortwave fluxes play an important role from May to June when the onset of sea ice melting occurs. The comparison between linearly detrended and nondetrended of each parameter indicates that significant impact of cloud and radiation properties on September sea ice retreat occurs over the Chukchi/Beaufort Sea at interannual time scale, especially over the period of 31 March to 29 April, while strongest climatological trends are found over the Laptev/Siberian Sea. NOAA MAPP under grant at the University of North Dakota [NA13OAR4310105]; NASA CERES project under grant at the University of Arizona [NNX17AC52G] 6 month embargo; First published: 21 February 2017 This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. |
author2 |
Univ Arizona, Dept Hydrol & Atmospher Sci Department of Hydrology & Atmospheric Sciences; University of Arizona; Tucson Arizona USA Department of Atmospheric Sciences; University of North Dakota; Grand Forks North Dakota USA |
format |
Article in Journal/Newspaper |
author |
Huang, Yiyi Dong, Xiquan Xi, Baike Dolinar, Erica K. Stanfield, Ryan E. |
spellingShingle |
Huang, Yiyi Dong, Xiquan Xi, Baike Dolinar, Erica K. Stanfield, Ryan E. The footprints of 16 year trends of Arctic springtime cloud and radiation properties on September sea ice retreat |
author_facet |
Huang, Yiyi Dong, Xiquan Xi, Baike Dolinar, Erica K. Stanfield, Ryan E. |
author_sort |
Huang, Yiyi |
title |
The footprints of 16 year trends of Arctic springtime cloud and radiation properties on September sea ice retreat |
title_short |
The footprints of 16 year trends of Arctic springtime cloud and radiation properties on September sea ice retreat |
title_full |
The footprints of 16 year trends of Arctic springtime cloud and radiation properties on September sea ice retreat |
title_fullStr |
The footprints of 16 year trends of Arctic springtime cloud and radiation properties on September sea ice retreat |
title_full_unstemmed |
The footprints of 16 year trends of Arctic springtime cloud and radiation properties on September sea ice retreat |
title_sort |
footprints of 16 year trends of arctic springtime cloud and radiation properties on september sea ice retreat |
publisher |
AMER GEOPHYSICAL UNION |
publishDate |
2017 |
url |
http://hdl.handle.net/10150/623224 https://doi.org/10.1002/2016JD026020 |
geographic |
Arctic Kara Sea Laptev Sea |
geographic_facet |
Arctic Kara Sea Laptev Sea |
genre |
Arctic Arctic Beaufort Sea Chukchi Kara Sea laptev Laptev Sea Sea ice |
genre_facet |
Arctic Arctic Beaufort Sea Chukchi Kara Sea laptev Laptev Sea Sea ice |
op_relation |
http://doi.wiley.com/10.1002/2016JD026020 The footprints of 16 year trends of Arctic springtime cloud and radiation properties on September sea ice retreat 2017, 122 (4):2179 Journal of Geophysical Research: Atmospheres 2169897X doi:10.1002/2016JD026020 http://hdl.handle.net/10150/623224 Journal of Geophysical Research: Atmospheres |
op_rights |
©2017. American Geophysical Union. All Rights Reserved. |
op_doi |
https://doi.org/10.1002/2016JD026020 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
122 |
container_issue |
4 |
container_start_page |
2179 |
op_container_end_page |
2193 |
_version_ |
1766297510079365120 |