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...

Full description

Bibliographic Details
Published in:Atmosphere
Main Authors: Mingyi Gu, G. W. K. Moore, Kevin Wood, Zhaomin Wang
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12111398
id ftmdpi:oai:mdpi.com:/2073-4433/12/11/1398/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2073-4433/12/11/1398/ 2023-08-20T04:04:35+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 agris 2021-10-25 application/pdf https://doi.org/10.3390/atmos12111398 EN eng Multidisciplinary Digital Publishing Institute Meteorology https://dx.doi.org/10.3390/atmos12111398 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 12; Issue 11; Pages: 1398 planetary boundary layer heights comparison icebreaker cruises dataset Chukchi and Beaufort Seas Text 2021 ftmdpi https://doi.org/10.3390/atmos12111398 2023-08-01T03:03:39Z 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. Text Arctic Arctic Ocean Beaufort Sea Chukchi Icebreaker MDPI Open Access Publishing Arctic Arctic Ocean Atmosphere 12 11 1398
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic planetary boundary layer heights comparison
icebreaker cruises dataset
Chukchi and Beaufort Seas
spellingShingle planetary boundary layer heights comparison
icebreaker cruises dataset
Chukchi and Beaufort Seas
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
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 Text
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 Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/atmos12111398
op_coverage agris
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; Volume 12; Issue 11; Pages: 1398
op_relation Meteorology
https://dx.doi.org/10.3390/atmos12111398
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos12111398
container_title Atmosphere
container_volume 12
container_issue 11
container_start_page 1398
_version_ 1774714965495644160