Spatial-Temporal Variability of Land Surface Dry Anomalies in Climatic Aspect: Biogeophysical Insight by Meteosat Observations and SVAT Modeling

The spatial-temporal variability of drought occurrence over Bulgaria is characterized based on long-term records (2007−2018) of Meteosat information and the SVAT model-derived soil moisture availability index (referred to root zone depth, SMAI). Land surface temperature according to the sa...

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Main Authors: Julia Stoyanova, Christo Georgiev, Plamen Neytchev, Andrey Kulishev
Format: Article
Language:English
Published: MDPI AG 2019-10-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/10/10/636
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spelling doaj-ea757c24948a421584910d37a8eb33282020-11-25T00:56:43ZengMDPI AGAtmosphere2073-44332019-10-01101063610.3390/atmos10100636atmos10100636Spatial-Temporal Variability of Land Surface Dry Anomalies in Climatic Aspect: Biogeophysical Insight by Meteosat Observations and SVAT ModelingJulia Stoyanova0Christo Georgiev1Plamen Neytchev2Andrey Kulishev3National Institute of Meteorology and Hydrology, 1784 Sofia, BulgariaNational Institute of Meteorology and Hydrology, 1784 Sofia, BulgariaNational Institute of Meteorology and Hydrology, 1784 Sofia, BulgariaNational Institute of Meteorology and Hydrology, 1784 Sofia, BulgariaThe spatial-temporal variability of drought occurrence over Bulgaria is characterized based on long-term records (2007−2018) of Meteosat information and the SVAT model-derived soil moisture availability index (referred to root zone depth, SMAI). Land surface temperature according to the satellite-derived Land Surface Analysis Satellite Application Facility Land Surface Temperature (LSASAF LST) product and SMAI were used to designate land surface state dry anomalies. The utility of LST for drought assessment is tested by statistical comparative analyses, applying two approaches, site-scale quantitative comparison, and evaluation of spatial-temporal consistency between SMAI and LST variability. Pearson correlation and regression modeling techniques were applied. The main results indicate for a synchronized behavior between SMAI and LST during dry spells, as follows: opposite mean seasonal course (March−October); high to strong negative monthly correlation for different microclimate regimes. Negative linear regressions between the anomalies of SMAI and LST (monthly mean), with a strong correlation in their spatial-temporal variability. Qualitative evaluation of spatial-temporal variability dynamics is analyzed using color maps. Drought-prone areas were identified on the bases of LST maps (monthly mean), and it is illustrated they are more vulnerable to vegetation burning as detected by the Meteosat FRP-PIXEL product. The current study provides an advanced framework for using LST retrievals based on IR satellite observations from the geostationary MSG satellite as an alternative tool to SMAI, whose calculation requires the input of many parameters that are not always available.https://www.mdpi.com/2073-4433/10/10/636dry land surface anomaliessoil moisture availability indexsvat modelingland surface temperaturesatellite observationsregional climatebiomass burning
collection DOAJ
language English
format Article
sources DOAJ
author Julia Stoyanova
Christo Georgiev
Plamen Neytchev
Andrey Kulishev
spellingShingle Julia Stoyanova
Christo Georgiev
Plamen Neytchev
Andrey Kulishev
Spatial-Temporal Variability of Land Surface Dry Anomalies in Climatic Aspect: Biogeophysical Insight by Meteosat Observations and SVAT Modeling
Atmosphere
dry land surface anomalies
soil moisture availability index
svat modeling
land surface temperature
satellite observations
regional climate
biomass burning
author_facet Julia Stoyanova
Christo Georgiev
Plamen Neytchev
Andrey Kulishev
author_sort Julia Stoyanova
title Spatial-Temporal Variability of Land Surface Dry Anomalies in Climatic Aspect: Biogeophysical Insight by Meteosat Observations and SVAT Modeling
title_short Spatial-Temporal Variability of Land Surface Dry Anomalies in Climatic Aspect: Biogeophysical Insight by Meteosat Observations and SVAT Modeling
title_full Spatial-Temporal Variability of Land Surface Dry Anomalies in Climatic Aspect: Biogeophysical Insight by Meteosat Observations and SVAT Modeling
title_fullStr Spatial-Temporal Variability of Land Surface Dry Anomalies in Climatic Aspect: Biogeophysical Insight by Meteosat Observations and SVAT Modeling
title_full_unstemmed Spatial-Temporal Variability of Land Surface Dry Anomalies in Climatic Aspect: Biogeophysical Insight by Meteosat Observations and SVAT Modeling
title_sort spatial-temporal variability of land surface dry anomalies in climatic aspect: biogeophysical insight by meteosat observations and svat modeling
publisher MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2019-10-01
description The spatial-temporal variability of drought occurrence over Bulgaria is characterized based on long-term records (2007−2018) of Meteosat information and the SVAT model-derived soil moisture availability index (referred to root zone depth, SMAI). Land surface temperature according to the satellite-derived Land Surface Analysis Satellite Application Facility Land Surface Temperature (LSASAF LST) product and SMAI were used to designate land surface state dry anomalies. The utility of LST for drought assessment is tested by statistical comparative analyses, applying two approaches, site-scale quantitative comparison, and evaluation of spatial-temporal consistency between SMAI and LST variability. Pearson correlation and regression modeling techniques were applied. The main results indicate for a synchronized behavior between SMAI and LST during dry spells, as follows: opposite mean seasonal course (March−October); high to strong negative monthly correlation for different microclimate regimes. Negative linear regressions between the anomalies of SMAI and LST (monthly mean), with a strong correlation in their spatial-temporal variability. Qualitative evaluation of spatial-temporal variability dynamics is analyzed using color maps. Drought-prone areas were identified on the bases of LST maps (monthly mean), and it is illustrated they are more vulnerable to vegetation burning as detected by the Meteosat FRP-PIXEL product. The current study provides an advanced framework for using LST retrievals based on IR satellite observations from the geostationary MSG satellite as an alternative tool to SMAI, whose calculation requires the input of many parameters that are not always available.
topic dry land surface anomalies
soil moisture availability index
svat modeling
land surface temperature
satellite observations
regional climate
biomass burning
url https://www.mdpi.com/2073-4433/10/10/636
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