Satellite-Derived Spatio-Temporal Distribution and Parameters of North Atlantic Polar Lows for 2015–2017

A list of North Atlantic polar lows was compiled for 2015–2017. A total of 131 polar lows were found by analyzing the Moderate Resolution Imaging Spectroradiometer (MODIS) infrared imagery and auxiliary information. The study region was additionally divided by the 20° W meridian to assess possible d...

Full description

Bibliographic Details
Published in:Atmosphere
Main Authors: Pavel Golubkin, Julia Smirnova, Leonid Bobylev
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12020224
id ftmdpi:oai:mdpi.com:/2073-4433/12/2/224/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2073-4433/12/2/224/ 2023-08-20T04:04:39+02:00 Satellite-Derived Spatio-Temporal Distribution and Parameters of North Atlantic Polar Lows for 2015–2017 Pavel Golubkin Julia Smirnova Leonid Bobylev agris 2021-02-06 application/pdf https://doi.org/10.3390/atmos12020224 EN eng Multidisciplinary Digital Publishing Institute Meteorology https://dx.doi.org/10.3390/atmos12020224 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 12; Issue 2; Pages: 224 polar lows polar mesoscale cyclones North Atlantic Arctic Text 2021 ftmdpi https://doi.org/10.3390/atmos12020224 2023-08-01T01:01:26Z A list of North Atlantic polar lows was compiled for 2015–2017. A total of 131 polar lows were found by analyzing the Moderate Resolution Imaging Spectroradiometer (MODIS) infrared imagery and auxiliary information. The study region was additionally divided by the 20° W meridian to assess possible differences in the polar lows occurring in the western and eastern parts of the region. The highest polar low activity was found over the Barents Sea and the northern Norwegian Sea. A large number of polar lows over this region were dual or multiple. When considering such systems as a single event, more polar lows were found in 2015 over the Labrador Sea and southern Davis Strait, which is the region with the second highest number of polar lows. High interannual variability of polar low frequency was noted, which was more pronounced in the western part of the region. During the analyzed period, the largest number of polar lows occurred in January for the western part of the region and in February for the eastern part. The main polar low parameters were similar within the region, with the mean values slightly higher in the western part of the region, but all extreme high values were observed in the eastern part. Text Arctic Atlantic Arctic Atlantic-Arctic Barents Sea Davis Strait Labrador Sea North Atlantic Norwegian Sea MDPI Open Access Publishing Arctic Barents Sea Norwegian Sea Atmosphere 12 2 224
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic polar lows
polar mesoscale cyclones
North Atlantic
Arctic
spellingShingle polar lows
polar mesoscale cyclones
North Atlantic
Arctic
Pavel Golubkin
Julia Smirnova
Leonid Bobylev
Satellite-Derived Spatio-Temporal Distribution and Parameters of North Atlantic Polar Lows for 2015–2017
topic_facet polar lows
polar mesoscale cyclones
North Atlantic
Arctic
description A list of North Atlantic polar lows was compiled for 2015–2017. A total of 131 polar lows were found by analyzing the Moderate Resolution Imaging Spectroradiometer (MODIS) infrared imagery and auxiliary information. The study region was additionally divided by the 20° W meridian to assess possible differences in the polar lows occurring in the western and eastern parts of the region. The highest polar low activity was found over the Barents Sea and the northern Norwegian Sea. A large number of polar lows over this region were dual or multiple. When considering such systems as a single event, more polar lows were found in 2015 over the Labrador Sea and southern Davis Strait, which is the region with the second highest number of polar lows. High interannual variability of polar low frequency was noted, which was more pronounced in the western part of the region. During the analyzed period, the largest number of polar lows occurred in January for the western part of the region and in February for the eastern part. The main polar low parameters were similar within the region, with the mean values slightly higher in the western part of the region, but all extreme high values were observed in the eastern part.
format Text
author Pavel Golubkin
Julia Smirnova
Leonid Bobylev
author_facet Pavel Golubkin
Julia Smirnova
Leonid Bobylev
author_sort Pavel Golubkin
title Satellite-Derived Spatio-Temporal Distribution and Parameters of North Atlantic Polar Lows for 2015–2017
title_short Satellite-Derived Spatio-Temporal Distribution and Parameters of North Atlantic Polar Lows for 2015–2017
title_full Satellite-Derived Spatio-Temporal Distribution and Parameters of North Atlantic Polar Lows for 2015–2017
title_fullStr Satellite-Derived Spatio-Temporal Distribution and Parameters of North Atlantic Polar Lows for 2015–2017
title_full_unstemmed Satellite-Derived Spatio-Temporal Distribution and Parameters of North Atlantic Polar Lows for 2015–2017
title_sort satellite-derived spatio-temporal distribution and parameters of north atlantic polar lows for 2015–2017
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/atmos12020224
op_coverage agris
geographic Arctic
Barents Sea
Norwegian Sea
geographic_facet Arctic
Barents Sea
Norwegian Sea
genre Arctic
Atlantic Arctic
Atlantic-Arctic
Barents Sea
Davis Strait
Labrador Sea
North Atlantic
Norwegian Sea
genre_facet Arctic
Atlantic Arctic
Atlantic-Arctic
Barents Sea
Davis Strait
Labrador Sea
North Atlantic
Norwegian Sea
op_source Atmosphere; Volume 12; Issue 2; Pages: 224
op_relation Meteorology
https://dx.doi.org/10.3390/atmos12020224
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos12020224
container_title Atmosphere
container_volume 12
container_issue 2
container_start_page 224
_version_ 1774715031134404608