Detecting Snowfall Events over the Arctic Using Optical and Microwave Satellite Measurements

The precipitation over the Arctic region is a difficult quantity to determine with high accuracy, as the in situ observation network is sparse, and current climate models, atmospheric reanalyses and direct satellite-based precipitation observations suffer from diverse difficulties that hinder the co...

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Main Authors: Jääskeläinen, Emmihenna, Kouki, Kerttu, Riihelä, Aku
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/hess-2023-278
https://hess.copernicus.org/preprints/hess-2023-278/
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spelling ftcopernicus:oai:publications.copernicus.org:hessd116149 2024-02-27T08:37:24+00:00 Detecting Snowfall Events over the Arctic Using Optical and Microwave Satellite Measurements Jääskeläinen, Emmihenna Kouki, Kerttu Riihelä, Aku 2024-01-26 application/pdf https://doi.org/10.5194/hess-2023-278 https://hess.copernicus.org/preprints/hess-2023-278/ eng eng doi:10.5194/hess-2023-278 https://hess.copernicus.org/preprints/hess-2023-278/ eISSN: 1607-7938 Text 2024 ftcopernicus https://doi.org/10.5194/hess-2023-278 2024-01-29T17:24:15Z The precipitation over the Arctic region is a difficult quantity to determine with high accuracy, as the in situ observation network is sparse, and current climate models, atmospheric reanalyses and direct satellite-based precipitation observations suffer from diverse difficulties that hinder the correct assessment of precipitation. We undertake a proof-of-concept investigation into how accurately optical satellite observations, namely Sentinel-2 surface reflectance-based grain size-connected specific surface area of snow (SSA), and microwave-based snow water equivalent (SWE) estimates can detect snowfalls over the Arctic. Here, we chose a limited area (a circle of 100 km radius around Luosto radar located in Northern Finland) and a short time period (covering March 2018) to test these data sources and their usability to this precipitation assessment problem. We classified differences between observations independently for SSA and SWE and compared the results to the radar-based snowfall information. These initial results are promising. Situations with snowfalls are classified with high recalls, 67 % for SWE and around 90 % for SSA when compared to radar-based data. Cases without snowfalls are more difficult to classify, the recall value for SWE is only 38 %, but for SSA the recall values are higher, varying from almost 60 % to over 70 %. These results indicate, that using optical and microwave-based satellite observations can be used to detect snowfall events over the Arctic. Text Arctic Northern Finland Copernicus Publications: E-Journals Arctic Luosto ENVELOPE(26.900,26.900,67.133,67.133)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The precipitation over the Arctic region is a difficult quantity to determine with high accuracy, as the in situ observation network is sparse, and current climate models, atmospheric reanalyses and direct satellite-based precipitation observations suffer from diverse difficulties that hinder the correct assessment of precipitation. We undertake a proof-of-concept investigation into how accurately optical satellite observations, namely Sentinel-2 surface reflectance-based grain size-connected specific surface area of snow (SSA), and microwave-based snow water equivalent (SWE) estimates can detect snowfalls over the Arctic. Here, we chose a limited area (a circle of 100 km radius around Luosto radar located in Northern Finland) and a short time period (covering March 2018) to test these data sources and their usability to this precipitation assessment problem. We classified differences between observations independently for SSA and SWE and compared the results to the radar-based snowfall information. These initial results are promising. Situations with snowfalls are classified with high recalls, 67 % for SWE and around 90 % for SSA when compared to radar-based data. Cases without snowfalls are more difficult to classify, the recall value for SWE is only 38 %, but for SSA the recall values are higher, varying from almost 60 % to over 70 %. These results indicate, that using optical and microwave-based satellite observations can be used to detect snowfall events over the Arctic.
format Text
author Jääskeläinen, Emmihenna
Kouki, Kerttu
Riihelä, Aku
spellingShingle Jääskeläinen, Emmihenna
Kouki, Kerttu
Riihelä, Aku
Detecting Snowfall Events over the Arctic Using Optical and Microwave Satellite Measurements
author_facet Jääskeläinen, Emmihenna
Kouki, Kerttu
Riihelä, Aku
author_sort Jääskeläinen, Emmihenna
title Detecting Snowfall Events over the Arctic Using Optical and Microwave Satellite Measurements
title_short Detecting Snowfall Events over the Arctic Using Optical and Microwave Satellite Measurements
title_full Detecting Snowfall Events over the Arctic Using Optical and Microwave Satellite Measurements
title_fullStr Detecting Snowfall Events over the Arctic Using Optical and Microwave Satellite Measurements
title_full_unstemmed Detecting Snowfall Events over the Arctic Using Optical and Microwave Satellite Measurements
title_sort detecting snowfall events over the arctic using optical and microwave satellite measurements
publishDate 2024
url https://doi.org/10.5194/hess-2023-278
https://hess.copernicus.org/preprints/hess-2023-278/
long_lat ENVELOPE(26.900,26.900,67.133,67.133)
geographic Arctic
Luosto
geographic_facet Arctic
Luosto
genre Arctic
Northern Finland
genre_facet Arctic
Northern Finland
op_source eISSN: 1607-7938
op_relation doi:10.5194/hess-2023-278
https://hess.copernicus.org/preprints/hess-2023-278/
op_doi https://doi.org/10.5194/hess-2023-278
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