Role of Horizontal Heat Advection in Arctic Surface Warming During Early Spring
Abstract Reanalysis data and numerical model are employed to uncover the mechanisms of spring (March–April) Arctic surface warming. Different from other seasons, little additional solar radiation absorption or seasonal heat storage release contributes to Arctic surface warming in spring. Both observ...
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ftdoajarticles:oai:doaj.org/article:5b6f0087b07042a2a81011302bd693c8 2024-09-15T17:52:47+00:00 Role of Horizontal Heat Advection in Arctic Surface Warming During Early Spring Haijin Dai 2023-08-01T00:00:00Z https://doi.org/10.1029/2023GL103234 https://doaj.org/article/5b6f0087b07042a2a81011302bd693c8 EN eng Wiley https://doi.org/10.1029/2023GL103234 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL103234 https://doaj.org/article/5b6f0087b07042a2a81011302bd693c8 Geophysical Research Letters, Vol 50, Iss 16, Pp n/a-n/a (2023) Arctic amplification atmospheric blocking spring Arctic warming Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL103234 2024-08-05T17:49:23Z Abstract Reanalysis data and numerical model are employed to uncover the mechanisms of spring (March–April) Arctic surface warming. Different from other seasons, little additional solar radiation absorption or seasonal heat storage release contributes to Arctic surface warming in spring. Both observation and numerical results suggest that horizontal heat advection dominates Arctic surface air warming. However, horizontal advection originates from lower latitudes instead of local energy redistribution as in other seasons. Furthermore, Arctic warming weakens the meridional potential vorticity gradient, which strengthens the synoptic atmospheric blocking event. As a result, more warm (cold) air is transported to higher (lower) latitudes along the edge of high pressure, which is an accumulation of atmospheric blocking events. The results suggest that anomalous meridional heat transport plays more important roles in Arctic surface warming when the anomalous radiative forcing is weak. Without being absorbed by the ocean, additional available energy induces strong Arctic springtime surface warming. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 16 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Arctic amplification atmospheric blocking spring Arctic warming Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Arctic amplification atmospheric blocking spring Arctic warming Geophysics. Cosmic physics QC801-809 Haijin Dai Role of Horizontal Heat Advection in Arctic Surface Warming During Early Spring |
topic_facet |
Arctic amplification atmospheric blocking spring Arctic warming Geophysics. Cosmic physics QC801-809 |
description |
Abstract Reanalysis data and numerical model are employed to uncover the mechanisms of spring (March–April) Arctic surface warming. Different from other seasons, little additional solar radiation absorption or seasonal heat storage release contributes to Arctic surface warming in spring. Both observation and numerical results suggest that horizontal heat advection dominates Arctic surface air warming. However, horizontal advection originates from lower latitudes instead of local energy redistribution as in other seasons. Furthermore, Arctic warming weakens the meridional potential vorticity gradient, which strengthens the synoptic atmospheric blocking event. As a result, more warm (cold) air is transported to higher (lower) latitudes along the edge of high pressure, which is an accumulation of atmospheric blocking events. The results suggest that anomalous meridional heat transport plays more important roles in Arctic surface warming when the anomalous radiative forcing is weak. Without being absorbed by the ocean, additional available energy induces strong Arctic springtime surface warming. |
format |
Article in Journal/Newspaper |
author |
Haijin Dai |
author_facet |
Haijin Dai |
author_sort |
Haijin Dai |
title |
Role of Horizontal Heat Advection in Arctic Surface Warming During Early Spring |
title_short |
Role of Horizontal Heat Advection in Arctic Surface Warming During Early Spring |
title_full |
Role of Horizontal Heat Advection in Arctic Surface Warming During Early Spring |
title_fullStr |
Role of Horizontal Heat Advection in Arctic Surface Warming During Early Spring |
title_full_unstemmed |
Role of Horizontal Heat Advection in Arctic Surface Warming During Early Spring |
title_sort |
role of horizontal heat advection in arctic surface warming during early spring |
publisher |
Wiley |
publishDate |
2023 |
url |
https://doi.org/10.1029/2023GL103234 https://doaj.org/article/5b6f0087b07042a2a81011302bd693c8 |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
Geophysical Research Letters, Vol 50, Iss 16, Pp n/a-n/a (2023) |
op_relation |
https://doi.org/10.1029/2023GL103234 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL103234 https://doaj.org/article/5b6f0087b07042a2a81011302bd693c8 |
op_doi |
https://doi.org/10.1029/2023GL103234 |
container_title |
Geophysical Research Letters |
container_volume |
50 |
container_issue |
16 |
_version_ |
1810294813091692544 |