Snow features on sea ice in the western Arctic Ocean during summer 2016

Arctic sea ice and its snow cover are important components of the cryosphere and the climate system. A series of in situ snow measurements were conducted during the seventh Chinese Arctic expedition in summer 2016 in the western Arctic Ocean. In this study, we made an analysis of snow features on Ar...

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Bibliographic Details
Published in:International Journal of Digital Earth
Main Authors: Qing Ji, Xiaoping Pang, Xi Zhao, Ruibo Lei
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2021
Subjects:
Online Access:https://doi.org/10.1080/17538947.2021.1966524
https://doaj.org/article/3ba339736d234dc0934e5ef06ae18e2a
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spelling ftdoajarticles:oai:doaj.org/article:3ba339736d234dc0934e5ef06ae18e2a 2023-10-09T21:47:59+02:00 Snow features on sea ice in the western Arctic Ocean during summer 2016 Qing Ji Xiaoping Pang Xi Zhao Ruibo Lei 2021-10-01T00:00:00Z https://doi.org/10.1080/17538947.2021.1966524 https://doaj.org/article/3ba339736d234dc0934e5ef06ae18e2a EN eng Taylor & Francis Group http://dx.doi.org/10.1080/17538947.2021.1966524 https://doaj.org/toc/1753-8947 https://doaj.org/toc/1753-8955 1753-8947 1753-8955 doi:10.1080/17538947.2021.1966524 https://doaj.org/article/3ba339736d234dc0934e5ef06ae18e2a International Journal of Digital Earth, Vol 14, Iss 10, Pp 1397-1410 (2021) snow cover snow grain size snow stratigraphy remote sensing Mathematical geography. Cartography GA1-1776 article 2021 ftdoajarticles https://doi.org/10.1080/17538947.2021.1966524 2023-09-24T00:35:56Z Arctic sea ice and its snow cover are important components of the cryosphere and the climate system. A series of in situ snow measurements were conducted during the seventh Chinese Arctic expedition in summer 2016 in the western Arctic Ocean. In this study, we made an analysis of snow features on Arctic sea ice based on in situ observations and the satellite-derived parameter of snow grain size from MODIS spectral reflectance data. Results indicate that snow depth on Arctic sea ice varied between 19 and 241 mm, with a mean value of 100 mm. The mean density of the snow was 340.4 kg/m3 during the expedition, which was higher than that reported in previous literature. The measurements revealed that a depth hoar layer was widely developed in the snow, accounting for 30%∼50% of the total snow depth. The equivalent snow grain size was small on the surface and large at the bottom in snow pits. The average relative error between MODIS-derived snow grain size and in situ measured surface snow grain size is 14.6%, indicating that remote sensing is a promising method to obtain large-scale information of snow grain size on Arctic sea ice. Article in Journal/Newspaper Arctic Arctic Ocean Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean International Journal of Digital Earth 14 10 1397 1410
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic snow cover
snow grain size
snow stratigraphy
remote sensing
Mathematical geography. Cartography
GA1-1776
spellingShingle snow cover
snow grain size
snow stratigraphy
remote sensing
Mathematical geography. Cartography
GA1-1776
Qing Ji
Xiaoping Pang
Xi Zhao
Ruibo Lei
Snow features on sea ice in the western Arctic Ocean during summer 2016
topic_facet snow cover
snow grain size
snow stratigraphy
remote sensing
Mathematical geography. Cartography
GA1-1776
description Arctic sea ice and its snow cover are important components of the cryosphere and the climate system. A series of in situ snow measurements were conducted during the seventh Chinese Arctic expedition in summer 2016 in the western Arctic Ocean. In this study, we made an analysis of snow features on Arctic sea ice based on in situ observations and the satellite-derived parameter of snow grain size from MODIS spectral reflectance data. Results indicate that snow depth on Arctic sea ice varied between 19 and 241 mm, with a mean value of 100 mm. The mean density of the snow was 340.4 kg/m3 during the expedition, which was higher than that reported in previous literature. The measurements revealed that a depth hoar layer was widely developed in the snow, accounting for 30%∼50% of the total snow depth. The equivalent snow grain size was small on the surface and large at the bottom in snow pits. The average relative error between MODIS-derived snow grain size and in situ measured surface snow grain size is 14.6%, indicating that remote sensing is a promising method to obtain large-scale information of snow grain size on Arctic sea ice.
format Article in Journal/Newspaper
author Qing Ji
Xiaoping Pang
Xi Zhao
Ruibo Lei
author_facet Qing Ji
Xiaoping Pang
Xi Zhao
Ruibo Lei
author_sort Qing Ji
title Snow features on sea ice in the western Arctic Ocean during summer 2016
title_short Snow features on sea ice in the western Arctic Ocean during summer 2016
title_full Snow features on sea ice in the western Arctic Ocean during summer 2016
title_fullStr Snow features on sea ice in the western Arctic Ocean during summer 2016
title_full_unstemmed Snow features on sea ice in the western Arctic Ocean during summer 2016
title_sort snow features on sea ice in the western arctic ocean during summer 2016
publisher Taylor & Francis Group
publishDate 2021
url https://doi.org/10.1080/17538947.2021.1966524
https://doaj.org/article/3ba339736d234dc0934e5ef06ae18e2a
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_source International Journal of Digital Earth, Vol 14, Iss 10, Pp 1397-1410 (2021)
op_relation http://dx.doi.org/10.1080/17538947.2021.1966524
https://doaj.org/toc/1753-8947
https://doaj.org/toc/1753-8955
1753-8947
1753-8955
doi:10.1080/17538947.2021.1966524
https://doaj.org/article/3ba339736d234dc0934e5ef06ae18e2a
op_doi https://doi.org/10.1080/17538947.2021.1966524
container_title International Journal of Digital Earth
container_volume 14
container_issue 10
container_start_page 1397
op_container_end_page 1410
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