Planetary Boundary Layer Heights from Cruises in Spring to Autumn Chukchi-Beaufort Sea Compared with ERA5

The planetary boundary layer height (PBLH) is a diagnostic field related to the effective heat capacity of the lower atmosphere, both stable and convective, and it constrains motion in this layer as well as impacts surface warming. Here, we used radiosonde data from five icebreaker cruises to the Ch...

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Bibliographic Details
Published in:Atmosphere
Main Authors: Mingyi Gu, G. W. K. Moore, Kevin Wood, Zhaomin Wang
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12111398
https://doaj.org/article/10af0939c6944a27bde9f526319118c5
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spelling ftdoajarticles:oai:doaj.org/article:10af0939c6944a27bde9f526319118c5 2023-05-15T15:05:43+02:00 Planetary Boundary Layer Heights from Cruises in Spring to Autumn Chukchi-Beaufort Sea Compared with ERA5 Mingyi Gu G. W. K. Moore Kevin Wood Zhaomin Wang 2021-10-01T00:00:00Z https://doi.org/10.3390/atmos12111398 https://doaj.org/article/10af0939c6944a27bde9f526319118c5 EN eng MDPI AG https://www.mdpi.com/2073-4433/12/11/1398 https://doaj.org/toc/2073-4433 doi:10.3390/atmos12111398 2073-4433 https://doaj.org/article/10af0939c6944a27bde9f526319118c5 Atmosphere, Vol 12, Iss 1398, p 1398 (2021) planetary boundary layer heights comparison icebreaker cruises dataset Chukchi and Beaufort Seas Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.3390/atmos12111398 2022-12-31T11:28:52Z The planetary boundary layer height (PBLH) is a diagnostic field related to the effective heat capacity of the lower atmosphere, both stable and convective, and it constrains motion in this layer as well as impacts surface warming. Here, we used radiosonde data from five icebreaker cruises to the Chukchi and Beaufort Seas during both spring and fall to derive PBLH using the bulk Ri method, which were then compared with results from ERA5 reanalysis. The ERA5 PBLH was similar to but slightly lower than the ship observations. Clear and consistent seasonal changes were found in both the observations and the reanalysis: PBLH decreased from mid-May to mid-June and subsequently increased after August. The comparison with ERA5 shows that, besides surface temperature, biases in PBLH are also a function of wind direction, suggesting that the availability of upwind observations is also important in representing processes active in the boundary layer over the Arctic Ocean. Article in Journal/Newspaper Arctic Arctic Ocean Beaufort Sea Chukchi Icebreaker Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Atmosphere 12 11 1398
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic planetary boundary layer heights comparison
icebreaker cruises dataset
Chukchi and Beaufort Seas
Meteorology. Climatology
QC851-999
spellingShingle planetary boundary layer heights comparison
icebreaker cruises dataset
Chukchi and Beaufort Seas
Meteorology. Climatology
QC851-999
Mingyi Gu
G. W. K. Moore
Kevin Wood
Zhaomin Wang
Planetary Boundary Layer Heights from Cruises in Spring to Autumn Chukchi-Beaufort Sea Compared with ERA5
topic_facet planetary boundary layer heights comparison
icebreaker cruises dataset
Chukchi and Beaufort Seas
Meteorology. Climatology
QC851-999
description The planetary boundary layer height (PBLH) is a diagnostic field related to the effective heat capacity of the lower atmosphere, both stable and convective, and it constrains motion in this layer as well as impacts surface warming. Here, we used radiosonde data from five icebreaker cruises to the Chukchi and Beaufort Seas during both spring and fall to derive PBLH using the bulk Ri method, which were then compared with results from ERA5 reanalysis. The ERA5 PBLH was similar to but slightly lower than the ship observations. Clear and consistent seasonal changes were found in both the observations and the reanalysis: PBLH decreased from mid-May to mid-June and subsequently increased after August. The comparison with ERA5 shows that, besides surface temperature, biases in PBLH are also a function of wind direction, suggesting that the availability of upwind observations is also important in representing processes active in the boundary layer over the Arctic Ocean.
format Article in Journal/Newspaper
author Mingyi Gu
G. W. K. Moore
Kevin Wood
Zhaomin Wang
author_facet Mingyi Gu
G. W. K. Moore
Kevin Wood
Zhaomin Wang
author_sort Mingyi Gu
title Planetary Boundary Layer Heights from Cruises in Spring to Autumn Chukchi-Beaufort Sea Compared with ERA5
title_short Planetary Boundary Layer Heights from Cruises in Spring to Autumn Chukchi-Beaufort Sea Compared with ERA5
title_full Planetary Boundary Layer Heights from Cruises in Spring to Autumn Chukchi-Beaufort Sea Compared with ERA5
title_fullStr Planetary Boundary Layer Heights from Cruises in Spring to Autumn Chukchi-Beaufort Sea Compared with ERA5
title_full_unstemmed Planetary Boundary Layer Heights from Cruises in Spring to Autumn Chukchi-Beaufort Sea Compared with ERA5
title_sort planetary boundary layer heights from cruises in spring to autumn chukchi-beaufort sea compared with era5
publisher MDPI AG
publishDate 2021
url https://doi.org/10.3390/atmos12111398
https://doaj.org/article/10af0939c6944a27bde9f526319118c5
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Beaufort Sea
Chukchi
Icebreaker
genre_facet Arctic
Arctic Ocean
Beaufort Sea
Chukchi
Icebreaker
op_source Atmosphere, Vol 12, Iss 1398, p 1398 (2021)
op_relation https://www.mdpi.com/2073-4433/12/11/1398
https://doaj.org/toc/2073-4433
doi:10.3390/atmos12111398
2073-4433
https://doaj.org/article/10af0939c6944a27bde9f526319118c5
op_doi https://doi.org/10.3390/atmos12111398
container_title Atmosphere
container_volume 12
container_issue 11
container_start_page 1398
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