Air/snow, snow/ice and ice/water interfaces detection from high-resolution vertical temperature profiles measured by ice mass-balance buoys on an Arctic lake

Snow and ice were monitored by thermistor-string-based Snow and Ice Mass Balance Array (SIMBA) in Lake Orajärvi in northern Finland. An existing automatic SIMBA-algorithm was further developed to derive air/snow, snow/ice and ice/water interfaces based on the SIMBA environment temperature (ET) profi...

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Main Authors: Yubing Cheng, Bin Cheng, Fei Zheng, Timo Vihma, Anna Kontu, Qinghua Yang, Zeliang Liao
Format: Article
Language:English
Published: Cambridge University Press 2020-12-01
Series:Annals of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0260305520000518/type/journal_article
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author Yubing Cheng
Bin Cheng
Fei Zheng
Timo Vihma
Anna Kontu
Qinghua Yang
Zeliang Liao
author_facet Yubing Cheng
Bin Cheng
Fei Zheng
Timo Vihma
Anna Kontu
Qinghua Yang
Zeliang Liao
author_sort Yubing Cheng
collection DOAJ
description Snow and ice were monitored by thermistor-string-based Snow and Ice Mass Balance Array (SIMBA) in Lake Orajärvi in northern Finland. An existing automatic SIMBA-algorithm was further developed to derive air/snow, snow/ice and ice/water interfaces based on the SIMBA environment temperature (ET) profiles. The identified interfaces agreed with in situ observations made in 2011/12 winter season. The method was capable to identify upward-moving snow/ice interface that was also visible from SIMBA heating temperature (HT) profiles, which responds to differences in the thermal diffusivities of air, snow, ice and water. The SIMBA data obtained in winters 2017/18 and 2018/19 were used to investigate snow and ice mass balance. An upward-moving snow/ice interface was detected as a result of meteoric ice (snow ice and superimposed ice) formation. Snow contributed to granular lake ice formation up to 40–55% of the total ice thickness on the seasonal mean. Heavy snowfalls and low air temperature in early winter are favourable for granular ice formation. The seasonal mean snow depth on nearby land was 2.7–2.9 times of that on the lake. The estimation of freeboard from snow and ice mass-balance measurement is sensitive to the snow density. Accurate ice freeboard calculation is still a challenge.
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spelling doaj.art-5baf70d14416498f8cdbfe27dd1571ec2023-03-09T12:27:41ZengCambridge University PressAnnals of Glaciology0260-30551727-56442020-12-016130931910.1017/aog.2020.51Air/snow, snow/ice and ice/water interfaces detection from high-resolution vertical temperature profiles measured by ice mass-balance buoys on an Arctic lakeYubing Cheng0Bin Cheng1https://orcid.org/0000-0001-8156-8412Fei Zheng2Timo Vihma3Anna Kontu4Qinghua Yang5https://orcid.org/0000-0002-7114-2036Zeliang Liao6Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China Finnish Meteorological Institute, Helsinki, Finland University of Chinese Academy of Sciences, Beijing, ChinaFinnish Meteorological Institute, Helsinki, FinlandInstitute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, ChinaFinnish Meteorological Institute, Helsinki, FinlandFinnish Meteorological Institute, Helsinki, FinlandSchool of Atmospheric Sciences and Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University, Guangzhou, China Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, ChinaSchool of Data and Computer Science, Sun Yat-sen University, Guangzhou, ChinaSnow and ice were monitored by thermistor-string-based Snow and Ice Mass Balance Array (SIMBA) in Lake Orajärvi in northern Finland. An existing automatic SIMBA-algorithm was further developed to derive air/snow, snow/ice and ice/water interfaces based on the SIMBA environment temperature (ET) profiles. The identified interfaces agreed with in situ observations made in 2011/12 winter season. The method was capable to identify upward-moving snow/ice interface that was also visible from SIMBA heating temperature (HT) profiles, which responds to differences in the thermal diffusivities of air, snow, ice and water. The SIMBA data obtained in winters 2017/18 and 2018/19 were used to investigate snow and ice mass balance. An upward-moving snow/ice interface was detected as a result of meteoric ice (snow ice and superimposed ice) formation. Snow contributed to granular lake ice formation up to 40–55% of the total ice thickness on the seasonal mean. Heavy snowfalls and low air temperature in early winter are favourable for granular ice formation. The seasonal mean snow depth on nearby land was 2.7–2.9 times of that on the lake. The estimation of freeboard from snow and ice mass-balance measurement is sensitive to the snow density. Accurate ice freeboard calculation is still a challenge.https://www.cambridge.org/core/product/identifier/S0260305520000518/type/journal_articleIce temperaturelake icesnow
spellingShingle Yubing Cheng
Bin Cheng
Fei Zheng
Timo Vihma
Anna Kontu
Qinghua Yang
Zeliang Liao
Air/snow, snow/ice and ice/water interfaces detection from high-resolution vertical temperature profiles measured by ice mass-balance buoys on an Arctic lake
Annals of Glaciology
Ice temperature
lake ice
snow
title Air/snow, snow/ice and ice/water interfaces detection from high-resolution vertical temperature profiles measured by ice mass-balance buoys on an Arctic lake
title_full Air/snow, snow/ice and ice/water interfaces detection from high-resolution vertical temperature profiles measured by ice mass-balance buoys on an Arctic lake
title_fullStr Air/snow, snow/ice and ice/water interfaces detection from high-resolution vertical temperature profiles measured by ice mass-balance buoys on an Arctic lake
title_full_unstemmed Air/snow, snow/ice and ice/water interfaces detection from high-resolution vertical temperature profiles measured by ice mass-balance buoys on an Arctic lake
title_short Air/snow, snow/ice and ice/water interfaces detection from high-resolution vertical temperature profiles measured by ice mass-balance buoys on an Arctic lake
title_sort air snow snow ice and ice water interfaces detection from high resolution vertical temperature profiles measured by ice mass balance buoys on an arctic lake
topic Ice temperature
lake ice
snow
url https://www.cambridge.org/core/product/identifier/S0260305520000518/type/journal_article
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