On the Critical Behaviour of Observed and Simulated Spatial Soil Moisture Fields during SGP97

The aircraft-based ESTAR soil moisture fields from the Southern Great Plains 1997 (SGP97) Hydrology Experiment are compared to the simulated ones obtained by Bertoldi et al. [1] with the GEOtop model [2], with a particular focus on their capability in capturing the critical point behaviour in their...

Full description

Bibliographic Details
Main Authors: Mekonnen Gebremichael, Antonella Di Domenico, Giovanni Laguardia
Format: Article
Language:English
Published: MDPI AG 2010-09-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/2/9/2097/
id doaj-06844ec9cd2146758925111628b9d1e7
record_format Article
spelling doaj-06844ec9cd2146758925111628b9d1e72020-11-25T00:58:22ZengMDPI AGRemote Sensing2072-42922010-09-01292097211010.3390/rs2092097On the Critical Behaviour of Observed and Simulated Spatial Soil Moisture Fields during SGP97Mekonnen GebremichaelAntonella Di DomenicoGiovanni LaguardiaThe aircraft-based ESTAR soil moisture fields from the Southern Great Plains 1997 (SGP97) Hydrology Experiment are compared to the simulated ones obtained by Bertoldi et al. [1] with the GEOtop model [2], with a particular focus on their capability in capturing the critical point behaviour in their space-time dynamics (see [3]). The critical point behaviour should denote the transition of soil moisture spatial patterns from an unorganized to organized appearance, as conditions become wetter. The study region is the Little Washita watershed, located in the southwest Oklahoma, in the Southern Great Plains region of the USA. The case study takes place from June 27 to July 16 and encompasses wetting and drying cycles allowing for exploring the behaviour under transient conditions. Results show that the critical probability value is 0.85 for GEOtop, and 0.80 for ESTAR. The GEOtop patterns appear more fragmented, being more reluctant to organization, as confirmed by the higher value of critical probability. Such behaviour is probably inherited by the model’s parameterization: land use and soil classes impose additional spatial structures to those related to the meteorological forcings and the hillslope morphology, driving to higher degrees of heterogeneity. http://www.mdpi.com/2072-4292/2/9/2097/soil moisturemicrowave radiometerland surface modelspatial patternspercolation theory
collection DOAJ
language English
format Article
sources DOAJ
author Mekonnen Gebremichael
Antonella Di Domenico
Giovanni Laguardia
spellingShingle Mekonnen Gebremichael
Antonella Di Domenico
Giovanni Laguardia
On the Critical Behaviour of Observed and Simulated Spatial Soil Moisture Fields during SGP97
Remote Sensing
soil moisture
microwave radiometer
land surface model
spatial patterns
percolation theory
author_facet Mekonnen Gebremichael
Antonella Di Domenico
Giovanni Laguardia
author_sort Mekonnen Gebremichael
title On the Critical Behaviour of Observed and Simulated Spatial Soil Moisture Fields during SGP97
title_short On the Critical Behaviour of Observed and Simulated Spatial Soil Moisture Fields during SGP97
title_full On the Critical Behaviour of Observed and Simulated Spatial Soil Moisture Fields during SGP97
title_fullStr On the Critical Behaviour of Observed and Simulated Spatial Soil Moisture Fields during SGP97
title_full_unstemmed On the Critical Behaviour of Observed and Simulated Spatial Soil Moisture Fields during SGP97
title_sort on the critical behaviour of observed and simulated spatial soil moisture fields during sgp97
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2010-09-01
description The aircraft-based ESTAR soil moisture fields from the Southern Great Plains 1997 (SGP97) Hydrology Experiment are compared to the simulated ones obtained by Bertoldi et al. [1] with the GEOtop model [2], with a particular focus on their capability in capturing the critical point behaviour in their space-time dynamics (see [3]). The critical point behaviour should denote the transition of soil moisture spatial patterns from an unorganized to organized appearance, as conditions become wetter. The study region is the Little Washita watershed, located in the southwest Oklahoma, in the Southern Great Plains region of the USA. The case study takes place from June 27 to July 16 and encompasses wetting and drying cycles allowing for exploring the behaviour under transient conditions. Results show that the critical probability value is 0.85 for GEOtop, and 0.80 for ESTAR. The GEOtop patterns appear more fragmented, being more reluctant to organization, as confirmed by the higher value of critical probability. Such behaviour is probably inherited by the model’s parameterization: land use and soil classes impose additional spatial structures to those related to the meteorological forcings and the hillslope morphology, driving to higher degrees of heterogeneity.
topic soil moisture
microwave radiometer
land surface model
spatial patterns
percolation theory
url http://www.mdpi.com/2072-4292/2/9/2097/
work_keys_str_mv AT mekonnengebremichael onthecriticalbehaviourofobservedandsimulatedspatialsoilmoisturefieldsduringsgp97
AT antonelladidomenico onthecriticalbehaviourofobservedandsimulatedspatialsoilmoisturefieldsduringsgp97
AT giovannilaguardia onthecriticalbehaviourofobservedandsimulatedspatialsoilmoisturefieldsduringsgp97
_version_ 1725220514147860480