Snow Albedo Seasonality and Trend from MODIS Sensor and Ground Data at Johnsons Glacier, Livingston Island, Maritime Antarctica

The aim of this work is to investigate whether snow albedo seasonality and trend under all sky conditions at Johnsons Glacier (Livingston Island, Antarctica) can be tracked using the Moderate Resolution Imaging Spectroradiometer (MODIS) snow albedo daily product MOD10A1. The time span is from Decemb...

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Main Authors: Javier F. Calleja, Alejandro Corbea-Pérez, Susana Fernández, Carmen Recondo, Juanjo Peón, Miguel Ángel de Pablo
Format: Article
Language:English
Published: MDPI AG 2019-08-01
Series:Sensors
Subjects:
Online Access:https://www.mdpi.com/1424-8220/19/16/3569
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spelling doaj-4f0adf84916847c99b0bf67b454886fb2020-11-25T01:17:11ZengMDPI AGSensors1424-82202019-08-011916356910.3390/s19163569s19163569Snow Albedo Seasonality and Trend from MODIS Sensor and Ground Data at Johnsons Glacier, Livingston Island, Maritime AntarcticaJavier F. Calleja0Alejandro Corbea-Pérez1Susana Fernández2Carmen Recondo3Juanjo Peón4Miguel Ángel de Pablo5Remote Sensing Applications (RSApps) Research Group, Department of Physics, University of Oviedo, 33007 Oviedo, SpainRemote Sensing Applications (RSApps) Research Group, Department of Mining Exploitation and Prospecting, University of Oviedo, 33600 Mieres, SpainMathematical Modelling (MOMA) Research Group, Department of Geology, University of Oviedo, 33005 Oviedo, SpainRemote Sensing Applications (RSApps) Research Group, Department of Mining Exploitation and Prospecting, University of Oviedo, 33600 Mieres, SpainRemote Sensing Applications (RSApps) Research Group, Department of Mining Exploitation and Prospecting, University of Oviedo, 33600 Mieres, SpainDepartment of Geology, Geography and Environment, University of Alcalá, 28805 Alcalá de Henares, SpainThe aim of this work is to investigate whether snow albedo seasonality and trend under all sky conditions at Johnsons Glacier (Livingston Island, Antarctica) can be tracked using the Moderate Resolution Imaging Spectroradiometer (MODIS) snow albedo daily product MOD10A1. The time span is from December 2006 to February 2015. As the MOD10A1 snow albedo product has never been used in Antarctica before, we also assess the performance for the MOD10A1 cloud mask. The motivation for this work is the need for a description of snow albedo under all sky conditions (including overcast days) using satellite data with mid-spatial resolution. In-situ albedo was filtered with a 5-day windowed moving average, while the MOD10A1 data were filtered using a maximum filter. Both in-situ and MOD10A1 data follow an exponential decay during the melting season, with a maximum decay of 0.049/0.094 day<sup>&#8722;1</sup> (in-situ/MOD10A1) for the 2006&#8722;2007 season and a minimum of 0.016/0.016 day<sup>&#8722;1</sup> for the 2009&#8722;2010 season. The duration of the decay varies from 85 days (2007&#8722;2008) to 167 days (2013&#8722;2014). Regarding the albedo trend, both data sets exhibit a slight increase of albedo, which may be explained by an increase of snowfall along with a decrease of snowmelt in the study area. Annual albedo increases of 0.2% and 0.7% are obtained for in-situ and MOD10A1 data, respectively, which amount to respective increases of 2% and 6% in the period 2006&#8722;2015. We conclude that MOD10A1 can be used to characterize snow albedo seasonality and trend on Livingston Island when filtered with a maximum filter.https://www.mdpi.com/1424-8220/19/16/3569albedoAntarcticaMODIS snow albedoin-situ albedoalbedo trendalbedo seasonality
collection DOAJ
language English
format Article
sources DOAJ
author Javier F. Calleja
Alejandro Corbea-Pérez
Susana Fernández
Carmen Recondo
Juanjo Peón
Miguel Ángel de Pablo
spellingShingle Javier F. Calleja
Alejandro Corbea-Pérez
Susana Fernández
Carmen Recondo
Juanjo Peón
Miguel Ángel de Pablo
Snow Albedo Seasonality and Trend from MODIS Sensor and Ground Data at Johnsons Glacier, Livingston Island, Maritime Antarctica
Sensors
albedo
Antarctica
MODIS snow albedo
in-situ albedo
albedo trend
albedo seasonality
author_facet Javier F. Calleja
Alejandro Corbea-Pérez
Susana Fernández
Carmen Recondo
Juanjo Peón
Miguel Ángel de Pablo
author_sort Javier F. Calleja
title Snow Albedo Seasonality and Trend from MODIS Sensor and Ground Data at Johnsons Glacier, Livingston Island, Maritime Antarctica
title_short Snow Albedo Seasonality and Trend from MODIS Sensor and Ground Data at Johnsons Glacier, Livingston Island, Maritime Antarctica
title_full Snow Albedo Seasonality and Trend from MODIS Sensor and Ground Data at Johnsons Glacier, Livingston Island, Maritime Antarctica
title_fullStr Snow Albedo Seasonality and Trend from MODIS Sensor and Ground Data at Johnsons Glacier, Livingston Island, Maritime Antarctica
title_full_unstemmed Snow Albedo Seasonality and Trend from MODIS Sensor and Ground Data at Johnsons Glacier, Livingston Island, Maritime Antarctica
title_sort snow albedo seasonality and trend from modis sensor and ground data at johnsons glacier, livingston island, maritime antarctica
publisher MDPI AG
series Sensors
issn 1424-8220
publishDate 2019-08-01
description The aim of this work is to investigate whether snow albedo seasonality and trend under all sky conditions at Johnsons Glacier (Livingston Island, Antarctica) can be tracked using the Moderate Resolution Imaging Spectroradiometer (MODIS) snow albedo daily product MOD10A1. The time span is from December 2006 to February 2015. As the MOD10A1 snow albedo product has never been used in Antarctica before, we also assess the performance for the MOD10A1 cloud mask. The motivation for this work is the need for a description of snow albedo under all sky conditions (including overcast days) using satellite data with mid-spatial resolution. In-situ albedo was filtered with a 5-day windowed moving average, while the MOD10A1 data were filtered using a maximum filter. Both in-situ and MOD10A1 data follow an exponential decay during the melting season, with a maximum decay of 0.049/0.094 day<sup>&#8722;1</sup> (in-situ/MOD10A1) for the 2006&#8722;2007 season and a minimum of 0.016/0.016 day<sup>&#8722;1</sup> for the 2009&#8722;2010 season. The duration of the decay varies from 85 days (2007&#8722;2008) to 167 days (2013&#8722;2014). Regarding the albedo trend, both data sets exhibit a slight increase of albedo, which may be explained by an increase of snowfall along with a decrease of snowmelt in the study area. Annual albedo increases of 0.2% and 0.7% are obtained for in-situ and MOD10A1 data, respectively, which amount to respective increases of 2% and 6% in the period 2006&#8722;2015. We conclude that MOD10A1 can be used to characterize snow albedo seasonality and trend on Livingston Island when filtered with a maximum filter.
topic albedo
Antarctica
MODIS snow albedo
in-situ albedo
albedo trend
albedo seasonality
url https://www.mdpi.com/1424-8220/19/16/3569
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