Comparing Measured Incoming Shortwave and Longwave Radiation on a Glacier Surface with Estimated Records from Satellite and Off-Glacier Observations: A Case Study for the Forni Glacier, Italy

The development of methods for quantifying meltwater from glaciated areas is very important for better management of water resources and because of the strong impact of current and expected climate change on the Alpine cryosphere. Radiative fluxes are the main melt-drivers, but they can generally no...

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Main Authors: Antonella Senese, Veronica Manara, Maurizio Maugeri, Guglielmina Adele Diolaiuti
Format: Article
Language:English
Published: MDPI AG 2020-11-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/22/3719
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author Antonella Senese
Veronica Manara
Maurizio Maugeri
Guglielmina Adele Diolaiuti
author_facet Antonella Senese
Veronica Manara
Maurizio Maugeri
Guglielmina Adele Diolaiuti
author_sort Antonella Senese
collection DOAJ
description The development of methods for quantifying meltwater from glaciated areas is very important for better management of water resources and because of the strong impact of current and expected climate change on the Alpine cryosphere. Radiative fluxes are the main melt-drivers, but they can generally not be derived from in situ measures because glaciers are usually located in remote areas where the number of meteorological stations is very low. For this reason, focusing, as a case study, on one of the few glaciers with a supraglacial automatic weather station (Forni Glacier), we investigated methods based on both satellite records and off-glacier surface observations to estimate incoming short- and long-wave radiation at the glacier surface (SW<sub>in</sub> and LW<sub>in</sub>). Specifically, for SW<sub>in</sub>, we considered CM SAF SARAH satellite gridded surface solar irradiance fields and data modeled by cloud transmissivity parametrized from both CM SAF COMET satellite cloud fractional cover fields and daily temperature range observed at the closest off-glacier station. We then used the latter two data sources to derive LW<sub>in</sub> too. Finally, we used the estimated SW<sub>in</sub> and LW<sub>in</sub> records to assess the errors obtained when introducing estimated rather than measured incoming radiation data to quantify glacier melting by means of an energy balance model. Our results suggest that estimated SW<sub>in</sub> and LW<sub>in</sub> records derived from satellite measures are in better agreement with in situ observations than estimated SW<sub>in</sub> and LW<sub>in</sub> records parametrized from observations performed at the closest off-glacier station. Moreover, we find that the former estimated records permit a significantly better quantification of glacier melting than the latter estimated ones.
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spelling doaj.art-b4fb87610591498e9edab62708adace72023-11-20T20:45:44ZengMDPI AGRemote Sensing2072-42922020-11-011222371910.3390/rs12223719Comparing Measured Incoming Shortwave and Longwave Radiation on a Glacier Surface with Estimated Records from Satellite and Off-Glacier Observations: A Case Study for the Forni Glacier, ItalyAntonella Senese0Veronica Manara1Maurizio Maugeri2Guglielmina Adele Diolaiuti3Department of Environmental Science and Policy, Università degli Studi di Milano, 20133 Milan, ItalyDepartment of Environmental Science and Policy, Università degli Studi di Milano, 20133 Milan, ItalyDepartment of Environmental Science and Policy, Università degli Studi di Milano, 20133 Milan, ItalyDepartment of Environmental Science and Policy, Università degli Studi di Milano, 20133 Milan, ItalyThe development of methods for quantifying meltwater from glaciated areas is very important for better management of water resources and because of the strong impact of current and expected climate change on the Alpine cryosphere. Radiative fluxes are the main melt-drivers, but they can generally not be derived from in situ measures because glaciers are usually located in remote areas where the number of meteorological stations is very low. For this reason, focusing, as a case study, on one of the few glaciers with a supraglacial automatic weather station (Forni Glacier), we investigated methods based on both satellite records and off-glacier surface observations to estimate incoming short- and long-wave radiation at the glacier surface (SW<sub>in</sub> and LW<sub>in</sub>). Specifically, for SW<sub>in</sub>, we considered CM SAF SARAH satellite gridded surface solar irradiance fields and data modeled by cloud transmissivity parametrized from both CM SAF COMET satellite cloud fractional cover fields and daily temperature range observed at the closest off-glacier station. We then used the latter two data sources to derive LW<sub>in</sub> too. Finally, we used the estimated SW<sub>in</sub> and LW<sub>in</sub> records to assess the errors obtained when introducing estimated rather than measured incoming radiation data to quantify glacier melting by means of an energy balance model. Our results suggest that estimated SW<sub>in</sub> and LW<sub>in</sub> records derived from satellite measures are in better agreement with in situ observations than estimated SW<sub>in</sub> and LW<sub>in</sub> records parametrized from observations performed at the closest off-glacier station. Moreover, we find that the former estimated records permit a significantly better quantification of glacier melting than the latter estimated ones.https://www.mdpi.com/2072-4292/12/22/3719radiative fluxescloud fractional coverdaily temperature rangesatellite dataSARAHCOMET
spellingShingle Antonella Senese
Veronica Manara
Maurizio Maugeri
Guglielmina Adele Diolaiuti
Comparing Measured Incoming Shortwave and Longwave Radiation on a Glacier Surface with Estimated Records from Satellite and Off-Glacier Observations: A Case Study for the Forni Glacier, Italy
Remote Sensing
radiative fluxes
cloud fractional cover
daily temperature range
satellite data
SARAH
COMET
title Comparing Measured Incoming Shortwave and Longwave Radiation on a Glacier Surface with Estimated Records from Satellite and Off-Glacier Observations: A Case Study for the Forni Glacier, Italy
title_full Comparing Measured Incoming Shortwave and Longwave Radiation on a Glacier Surface with Estimated Records from Satellite and Off-Glacier Observations: A Case Study for the Forni Glacier, Italy
title_fullStr Comparing Measured Incoming Shortwave and Longwave Radiation on a Glacier Surface with Estimated Records from Satellite and Off-Glacier Observations: A Case Study for the Forni Glacier, Italy
title_full_unstemmed Comparing Measured Incoming Shortwave and Longwave Radiation on a Glacier Surface with Estimated Records from Satellite and Off-Glacier Observations: A Case Study for the Forni Glacier, Italy
title_short Comparing Measured Incoming Shortwave and Longwave Radiation on a Glacier Surface with Estimated Records from Satellite and Off-Glacier Observations: A Case Study for the Forni Glacier, Italy
title_sort comparing measured incoming shortwave and longwave radiation on a glacier surface with estimated records from satellite and off glacier observations a case study for the forni glacier italy
topic radiative fluxes
cloud fractional cover
daily temperature range
satellite data
SARAH
COMET
url https://www.mdpi.com/2072-4292/12/22/3719
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