Analysis of a Sea Fog Episode at King George Island, Antarctica

In this study, a marine fog episode at King George Island off the Antarctic Peninsula from 26−30 January 2017 was investigated using surface observations, upper-air soundings, and re-analysis data as well as the air mass backward trajectory method. The marine fog episode resulted from an approaching...
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Autor*in:	Jianqiao Chen [verfasserIn] Bo Han [verfasserIn] Qinghua Yang [verfasserIn] Lixin Wei [verfasserIn] Yindong Zeng [verfasserIn] Renhao Wu [verfasserIn] Lin Zhang [verfasserIn] Zhuoming Ding [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Schlagwörter:	marine fog air-sea temperature difference air-sea interaction backward trajectory

Übergeordnetes Werk:	In: Atmosphere - MDPI AG, 2011, 10(2019), 10, p 585
Übergeordnetes Werk:	volume:10 ; year:2019 ; number:10, p 585

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/atmos10100585

Katalog-ID:	DOAJ044418655

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520			\|a In this study, a marine fog episode at King George Island off the Antarctic Peninsula from 26−30 January 2017 was investigated using surface observations, upper-air soundings, and re-analysis data as well as the air mass backward trajectory method. The marine fog episode resulted from an approaching low-pressure system, was maintained at high wind speeds, and quickly dissipated when the low-pressure system passed the observation site. During this episode, cloud lay existed above the fog and stratus, the atmosphere was stably stratified for 1600 m, and the air close to the surface was more mixed than air in the upper layer. The air-sea temperature difference (ASTD) of 1−2 °C and a strong surface wind parallel to the gradient of SST were two important factors in the formation and maintenance of the marine fog near the Antarctic region. The convergence of flux for both water vapor and heat during the fog episode was also discussed.
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allfields	10.3390/atmos10100585 doi (DE-627)DOAJ044418655 (DE-599)DOAJ96a63923b21145089dd546a45e6fdb86 DE-627 ger DE-627 rakwb eng QC851-999 Jianqiao Chen verfasserin aut Analysis of a Sea Fog Episode at King George Island, Antarctica 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier In this study, a marine fog episode at King George Island off the Antarctic Peninsula from 26−30 January 2017 was investigated using surface observations, upper-air soundings, and re-analysis data as well as the air mass backward trajectory method. The marine fog episode resulted from an approaching low-pressure system, was maintained at high wind speeds, and quickly dissipated when the low-pressure system passed the observation site. During this episode, cloud lay existed above the fog and stratus, the atmosphere was stably stratified for 1600 m, and the air close to the surface was more mixed than air in the upper layer. The air-sea temperature difference (ASTD) of 1−2 °C and a strong surface wind parallel to the gradient of SST were two important factors in the formation and maintenance of the marine fog near the Antarctic region. The convergence of flux for both water vapor and heat during the fog episode was also discussed. marine fog air-sea temperature difference air-sea interaction backward trajectory Meteorology. Climatology Bo Han verfasserin aut Qinghua Yang verfasserin aut Lixin Wei verfasserin aut Yindong Zeng verfasserin aut Renhao Wu verfasserin aut Lin Zhang verfasserin aut Zhuoming Ding verfasserin aut In Atmosphere MDPI AG, 2011 10(2019), 10, p 585 (DE-627)657584010 (DE-600)2605928-9 20734433 nnns volume:10 year:2019 number:10, p 585 https://doi.org/10.3390/atmos10100585 kostenfrei https://doaj.org/article/96a63923b21145089dd546a45e6fdb86 kostenfrei https://www.mdpi.com/2073-4433/10/10/585 kostenfrei https://doaj.org/toc/2073-4433 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 10, p 585
spelling	10.3390/atmos10100585 doi (DE-627)DOAJ044418655 (DE-599)DOAJ96a63923b21145089dd546a45e6fdb86 DE-627 ger DE-627 rakwb eng QC851-999 Jianqiao Chen verfasserin aut Analysis of a Sea Fog Episode at King George Island, Antarctica 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier In this study, a marine fog episode at King George Island off the Antarctic Peninsula from 26−30 January 2017 was investigated using surface observations, upper-air soundings, and re-analysis data as well as the air mass backward trajectory method. The marine fog episode resulted from an approaching low-pressure system, was maintained at high wind speeds, and quickly dissipated when the low-pressure system passed the observation site. During this episode, cloud lay existed above the fog and stratus, the atmosphere was stably stratified for 1600 m, and the air close to the surface was more mixed than air in the upper layer. The air-sea temperature difference (ASTD) of 1−2 °C and a strong surface wind parallel to the gradient of SST were two important factors in the formation and maintenance of the marine fog near the Antarctic region. The convergence of flux for both water vapor and heat during the fog episode was also discussed. marine fog air-sea temperature difference air-sea interaction backward trajectory Meteorology. Climatology Bo Han verfasserin aut Qinghua Yang verfasserin aut Lixin Wei verfasserin aut Yindong Zeng verfasserin aut Renhao Wu verfasserin aut Lin Zhang verfasserin aut Zhuoming Ding verfasserin aut In Atmosphere MDPI AG, 2011 10(2019), 10, p 585 (DE-627)657584010 (DE-600)2605928-9 20734433 nnns volume:10 year:2019 number:10, p 585 https://doi.org/10.3390/atmos10100585 kostenfrei https://doaj.org/article/96a63923b21145089dd546a45e6fdb86 kostenfrei https://www.mdpi.com/2073-4433/10/10/585 kostenfrei https://doaj.org/toc/2073-4433 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 10, p 585
allfields_unstemmed	10.3390/atmos10100585 doi (DE-627)DOAJ044418655 (DE-599)DOAJ96a63923b21145089dd546a45e6fdb86 DE-627 ger DE-627 rakwb eng QC851-999 Jianqiao Chen verfasserin aut Analysis of a Sea Fog Episode at King George Island, Antarctica 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier In this study, a marine fog episode at King George Island off the Antarctic Peninsula from 26−30 January 2017 was investigated using surface observations, upper-air soundings, and re-analysis data as well as the air mass backward trajectory method. The marine fog episode resulted from an approaching low-pressure system, was maintained at high wind speeds, and quickly dissipated when the low-pressure system passed the observation site. During this episode, cloud lay existed above the fog and stratus, the atmosphere was stably stratified for 1600 m, and the air close to the surface was more mixed than air in the upper layer. The air-sea temperature difference (ASTD) of 1−2 °C and a strong surface wind parallel to the gradient of SST were two important factors in the formation and maintenance of the marine fog near the Antarctic region. The convergence of flux for both water vapor and heat during the fog episode was also discussed. marine fog air-sea temperature difference air-sea interaction backward trajectory Meteorology. Climatology Bo Han verfasserin aut Qinghua Yang verfasserin aut Lixin Wei verfasserin aut Yindong Zeng verfasserin aut Renhao Wu verfasserin aut Lin Zhang verfasserin aut Zhuoming Ding verfasserin aut In Atmosphere MDPI AG, 2011 10(2019), 10, p 585 (DE-627)657584010 (DE-600)2605928-9 20734433 nnns volume:10 year:2019 number:10, p 585 https://doi.org/10.3390/atmos10100585 kostenfrei https://doaj.org/article/96a63923b21145089dd546a45e6fdb86 kostenfrei https://www.mdpi.com/2073-4433/10/10/585 kostenfrei https://doaj.org/toc/2073-4433 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 10, p 585
allfieldsGer	10.3390/atmos10100585 doi (DE-627)DOAJ044418655 (DE-599)DOAJ96a63923b21145089dd546a45e6fdb86 DE-627 ger DE-627 rakwb eng QC851-999 Jianqiao Chen verfasserin aut Analysis of a Sea Fog Episode at King George Island, Antarctica 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier In this study, a marine fog episode at King George Island off the Antarctic Peninsula from 26−30 January 2017 was investigated using surface observations, upper-air soundings, and re-analysis data as well as the air mass backward trajectory method. The marine fog episode resulted from an approaching low-pressure system, was maintained at high wind speeds, and quickly dissipated when the low-pressure system passed the observation site. During this episode, cloud lay existed above the fog and stratus, the atmosphere was stably stratified for 1600 m, and the air close to the surface was more mixed than air in the upper layer. The air-sea temperature difference (ASTD) of 1−2 °C and a strong surface wind parallel to the gradient of SST were two important factors in the formation and maintenance of the marine fog near the Antarctic region. The convergence of flux for both water vapor and heat during the fog episode was also discussed. marine fog air-sea temperature difference air-sea interaction backward trajectory Meteorology. Climatology Bo Han verfasserin aut Qinghua Yang verfasserin aut Lixin Wei verfasserin aut Yindong Zeng verfasserin aut Renhao Wu verfasserin aut Lin Zhang verfasserin aut Zhuoming Ding verfasserin aut In Atmosphere MDPI AG, 2011 10(2019), 10, p 585 (DE-627)657584010 (DE-600)2605928-9 20734433 nnns volume:10 year:2019 number:10, p 585 https://doi.org/10.3390/atmos10100585 kostenfrei https://doaj.org/article/96a63923b21145089dd546a45e6fdb86 kostenfrei https://www.mdpi.com/2073-4433/10/10/585 kostenfrei https://doaj.org/toc/2073-4433 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 10, p 585
allfieldsSound	10.3390/atmos10100585 doi (DE-627)DOAJ044418655 (DE-599)DOAJ96a63923b21145089dd546a45e6fdb86 DE-627 ger DE-627 rakwb eng QC851-999 Jianqiao Chen verfasserin aut Analysis of a Sea Fog Episode at King George Island, Antarctica 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier In this study, a marine fog episode at King George Island off the Antarctic Peninsula from 26−30 January 2017 was investigated using surface observations, upper-air soundings, and re-analysis data as well as the air mass backward trajectory method. The marine fog episode resulted from an approaching low-pressure system, was maintained at high wind speeds, and quickly dissipated when the low-pressure system passed the observation site. During this episode, cloud lay existed above the fog and stratus, the atmosphere was stably stratified for 1600 m, and the air close to the surface was more mixed than air in the upper layer. The air-sea temperature difference (ASTD) of 1−2 °C and a strong surface wind parallel to the gradient of SST were two important factors in the formation and maintenance of the marine fog near the Antarctic region. The convergence of flux for both water vapor and heat during the fog episode was also discussed. marine fog air-sea temperature difference air-sea interaction backward trajectory Meteorology. Climatology Bo Han verfasserin aut Qinghua Yang verfasserin aut Lixin Wei verfasserin aut Yindong Zeng verfasserin aut Renhao Wu verfasserin aut Lin Zhang verfasserin aut Zhuoming Ding verfasserin aut In Atmosphere MDPI AG, 2011 10(2019), 10, p 585 (DE-627)657584010 (DE-600)2605928-9 20734433 nnns volume:10 year:2019 number:10, p 585 https://doi.org/10.3390/atmos10100585 kostenfrei https://doaj.org/article/96a63923b21145089dd546a45e6fdb86 kostenfrei https://www.mdpi.com/2073-4433/10/10/585 kostenfrei https://doaj.org/toc/2073-4433 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 10, p 585
language	English
source	In Atmosphere 10(2019), 10, p 585 volume:10 year:2019 number:10, p 585
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container_title	Atmosphere
authorswithroles_txt_mv	Jianqiao Chen @@aut@@ Bo Han @@aut@@ Qinghua Yang @@aut@@ Lixin Wei @@aut@@ Yindong Zeng @@aut@@ Renhao Wu @@aut@@ Lin Zhang @@aut@@ Zhuoming Ding @@aut@@
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callnumber-first	Q - Science
author	Jianqiao Chen
spellingShingle	Jianqiao Chen misc QC851-999 misc marine fog misc air-sea temperature difference misc air-sea interaction misc backward trajectory misc Meteorology. Climatology Analysis of a Sea Fog Episode at King George Island, Antarctica
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topic_title	QC851-999 Analysis of a Sea Fog Episode at King George Island, Antarctica marine fog air-sea temperature difference air-sea interaction backward trajectory
topic	misc QC851-999 misc marine fog misc air-sea temperature difference misc air-sea interaction misc backward trajectory misc Meteorology. Climatology
topic_unstemmed	misc QC851-999 misc marine fog misc air-sea temperature difference misc air-sea interaction misc backward trajectory misc Meteorology. Climatology
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title	Analysis of a Sea Fog Episode at King George Island, Antarctica
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title_full	Analysis of a Sea Fog Episode at King George Island, Antarctica
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title_sort	analysis of a sea fog episode at king george island, antarctica
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title_auth	Analysis of a Sea Fog Episode at King George Island, Antarctica
abstract	In this study, a marine fog episode at King George Island off the Antarctic Peninsula from 26−30 January 2017 was investigated using surface observations, upper-air soundings, and re-analysis data as well as the air mass backward trajectory method. The marine fog episode resulted from an approaching low-pressure system, was maintained at high wind speeds, and quickly dissipated when the low-pressure system passed the observation site. During this episode, cloud lay existed above the fog and stratus, the atmosphere was stably stratified for 1600 m, and the air close to the surface was more mixed than air in the upper layer. The air-sea temperature difference (ASTD) of 1−2 °C and a strong surface wind parallel to the gradient of SST were two important factors in the formation and maintenance of the marine fog near the Antarctic region. The convergence of flux for both water vapor and heat during the fog episode was also discussed.
abstractGer	In this study, a marine fog episode at King George Island off the Antarctic Peninsula from 26−30 January 2017 was investigated using surface observations, upper-air soundings, and re-analysis data as well as the air mass backward trajectory method. The marine fog episode resulted from an approaching low-pressure system, was maintained at high wind speeds, and quickly dissipated when the low-pressure system passed the observation site. During this episode, cloud lay existed above the fog and stratus, the atmosphere was stably stratified for 1600 m, and the air close to the surface was more mixed than air in the upper layer. The air-sea temperature difference (ASTD) of 1−2 °C and a strong surface wind parallel to the gradient of SST were two important factors in the formation and maintenance of the marine fog near the Antarctic region. The convergence of flux for both water vapor and heat during the fog episode was also discussed.
abstract_unstemmed	In this study, a marine fog episode at King George Island off the Antarctic Peninsula from 26−30 January 2017 was investigated using surface observations, upper-air soundings, and re-analysis data as well as the air mass backward trajectory method. The marine fog episode resulted from an approaching low-pressure system, was maintained at high wind speeds, and quickly dissipated when the low-pressure system passed the observation site. During this episode, cloud lay existed above the fog and stratus, the atmosphere was stably stratified for 1600 m, and the air close to the surface was more mixed than air in the upper layer. The air-sea temperature difference (ASTD) of 1−2 °C and a strong surface wind parallel to the gradient of SST were two important factors in the formation and maintenance of the marine fog near the Antarctic region. The convergence of flux for both water vapor and heat during the fog episode was also discussed.
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container_issue	10, p 585
title_short	Analysis of a Sea Fog Episode at King George Island, Antarctica
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up_date	2024-07-03T22:54:59.286Z
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Analysis of a Sea Fog Episode at King George Island, Antarctica

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