Analysis of surface soil moisture patterns in agricultural landscapes using Empirical Orthogonal Functions

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Title:Main Title: Analysis of surface soil moisture patterns in agricultural landscapes using Empirical Orthogonal Functions
Description:Abstract: Soil moisture is one of the fundamental variables in hydrology, meteorology and agriculture. Nevertheless, its spatio-temporal patterns in agriculturally used landscapes that are affected by multiple natural (rainfall, soil, topography etc.) and agronomic (fertilisation, soil management etc.) factors are often not well known. The aim of this study is to determine the dominant factors governing the spatiotemporal patterns of surface soil moisture in a grassland and an arable test site that are located within the Rur catchment in Western Germany. Surface soil moisture (0–6 cm) was measured in an approx. 50×50m grid during 14 and 17 measurement campaigns (May 2007 to November 2008) in both test sites. To analyse the spatio-temporal patterns of surface soil moisture, an Empirical Orthogonal Function (EOF) analysis was applied and the results were correlated with parameters derived from topography, soil, vegetation and land management to link the patterns to related factors and processes. For the grassland test site, the analysis resulted in one significant spatial structure (first EOF), which explained 57.5% of the spatial variability connected to soil properties and topography. The statistical weight of the first spatial EOF is stronger on wet days. The highest temporal variability can be found in locations with a high percentage of soil organic carbon (SOC). For the arable test site, the analysis resulted in two significant spatial structures, the first EOF, which explained 38.4% of the spatial variability, and showed a highly significant correlation to soil properties, namely soil texture and soil stone content. The second EOF, which explained 28.3% of the spatial variability, is linked to differences in land management. The soil moisture in the arable test site varied more strongly during dry and wet periods at locations with low porosity. The method applied is capable of identifying the dominant parameters controlling spatio-temporal patterns of surface soil moisture without being affected by single random processes, even in intensively managed agricultural areas.
Identifier:10.5194/hess-14-751-2010 (DOI)
Responsible Party
Creators:Wolfgang Korres (Author), Christian N. Koyama (Author), Peter Fiener (Author), Karl Schneider (Author)
Publisher:European Geosciences Union
Publication Year:2013
Topic
TR32 Topic:Soil
Related Subproject:C3
Subjects:Keywords: Soil Moisture, Agriculture, Hydrology
File Details
Filename:2010_Korres_HESS.pdf
Data Type:Text - Article
Size:14 Pages
File Size:417 KB
Dates:Accepted: 14.04.2010
Issued: 12.05.2010
Mime Type:application/pdf
Data Format:PDF
Language:English
Status:Completed
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Download Permission:Only Project Members
General Access and Use Conditions:For internal use only
Access Limitations:For internal use only
Licence:[TR32DB] Data policy agreement
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Specific Information - Publication
Publication Status:Published
Review Status:Peer reviewed
Publication Type:Article
Article Type:Journal
Source:Hydrology and Earth System Sciences
Source Website:www.hydrol-earth-syst-sci.net
Volume:14
Number of Pages:14 (751 - 764)
Metadata Details
Metadata Creator:Wolfgang Korres
Metadata Created:02.12.2013
Metadata Last Updated:02.12.2013
Subproject:C3
Funding Phase:1
Metadata Language:English
Metadata Version:V50
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