Atmospheric circulation conditions and snowy weather in the Southern Alps: Case of the Isola 2000 weather station

This paper focuses on the relationship between atmospheric circulation and solid precipitation (SP) happening in the weather station of Isola 2000. Located in the French department of the Alpes-Maritimes at an altitude of 1912 m, it has the oldest series of daily SP and snow depth (SD) observations...

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Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=17338
http://id.nii.ac.jp/1291/00017202/
id ftnipr:oai:nipr.repo.nii.ac.jp:00017338
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00017338 2023-06-11T04:13:11+02:00 Atmospheric circulation conditions and snowy weather in the Southern Alps: Case of the Isola 2000 weather station 2023-03 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=17338 http://id.nii.ac.jp/1291/00017202/ en eng https://doi.org/10.1016/j.polar.2022.100922 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=17338 http://id.nii.ac.jp/1291/00017202/ Polar Science, 100922(2023-03) 18739652 Climate change Solid precipitation Snow depth ERA-INTERIM reanalysis Atmospheric circulation Southern Alps Journal Article 2023 ftnipr https://doi.org/10.1016/j.polar.2022.100922 2023-04-29T19:34:29Z This paper focuses on the relationship between atmospheric circulation and solid precipitation (SP) happening in the weather station of Isola 2000. Located in the French department of the Alpes-Maritimes at an altitude of 1912 m, it has the oldest series of daily SP and snow depth (SD) observations from the department. Study has two objectives, analyzed past orientations concerning air temperature, SP and SD, then, characterizes and explains the atmospheric circulation condition producing SP. Results show a warming of air temperature since the early 2000s, counterintuitive accompanied by an increase in the frequency of SP and a larger thickness of SD. In addition, by crossing SP observations with ERA-INTERIM reanalysis (EI-R), seven covariations have been measured: vertical velocity 700 hPa; specific humidity 850 hPa; sea level pressure; air temperature 850 hPa; geopotential height 700 hPa; U-component of wind 700 hPa, V-component of wind 700 hPa. The mapping of these variables shows two types of atmospheric circulation implicated in SP: westerly cyclonic circulation, producing SP in the range of 1–5 cm and 6–20 cm; southern circulation with a depression focused on Iceland and a trough on Western Europe, causing SP in the range of 21–40 cm and 41–93 cm. Article in Journal/Newspaper Iceland Polar Science Polar Science National Institute of Polar Research Repository, Japan Polar Science 35 100922
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Climate change
Solid precipitation
Snow depth
ERA-INTERIM reanalysis
Atmospheric circulation
Southern Alps
spellingShingle Climate change
Solid precipitation
Snow depth
ERA-INTERIM reanalysis
Atmospheric circulation
Southern Alps
Atmospheric circulation conditions and snowy weather in the Southern Alps: Case of the Isola 2000 weather station
topic_facet Climate change
Solid precipitation
Snow depth
ERA-INTERIM reanalysis
Atmospheric circulation
Southern Alps
description This paper focuses on the relationship between atmospheric circulation and solid precipitation (SP) happening in the weather station of Isola 2000. Located in the French department of the Alpes-Maritimes at an altitude of 1912 m, it has the oldest series of daily SP and snow depth (SD) observations from the department. Study has two objectives, analyzed past orientations concerning air temperature, SP and SD, then, characterizes and explains the atmospheric circulation condition producing SP. Results show a warming of air temperature since the early 2000s, counterintuitive accompanied by an increase in the frequency of SP and a larger thickness of SD. In addition, by crossing SP observations with ERA-INTERIM reanalysis (EI-R), seven covariations have been measured: vertical velocity 700 hPa; specific humidity 850 hPa; sea level pressure; air temperature 850 hPa; geopotential height 700 hPa; U-component of wind 700 hPa, V-component of wind 700 hPa. The mapping of these variables shows two types of atmospheric circulation implicated in SP: westerly cyclonic circulation, producing SP in the range of 1–5 cm and 6–20 cm; southern circulation with a depression focused on Iceland and a trough on Western Europe, causing SP in the range of 21–40 cm and 41–93 cm.
format Article in Journal/Newspaper
title Atmospheric circulation conditions and snowy weather in the Southern Alps: Case of the Isola 2000 weather station
title_short Atmospheric circulation conditions and snowy weather in the Southern Alps: Case of the Isola 2000 weather station
title_full Atmospheric circulation conditions and snowy weather in the Southern Alps: Case of the Isola 2000 weather station
title_fullStr Atmospheric circulation conditions and snowy weather in the Southern Alps: Case of the Isola 2000 weather station
title_full_unstemmed Atmospheric circulation conditions and snowy weather in the Southern Alps: Case of the Isola 2000 weather station
title_sort atmospheric circulation conditions and snowy weather in the southern alps: case of the isola 2000 weather station
publishDate 2023
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=17338
http://id.nii.ac.jp/1291/00017202/
genre Iceland
Polar Science
Polar Science
genre_facet Iceland
Polar Science
Polar Science
op_relation https://doi.org/10.1016/j.polar.2022.100922
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=17338
http://id.nii.ac.jp/1291/00017202/
Polar Science, 100922(2023-03)
18739652
op_doi https://doi.org/10.1016/j.polar.2022.100922
container_title Polar Science
container_volume 35
container_start_page 100922
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