Land Degradation Assessment Using Residual Trend Analysis of GIMMS NDVI3g, Soil Moisture and Rainfall in Sub-Saharan West Africa from 1982 to 2012

Areas affected by land degradation in Sub-Saharan West Africa between 1982 and 2012 are identified using time-series analysis of vegetation index data derived from satellites. The residual trend (RESTREND) of a Normalized Difference Vegetation Index (NDVI) time-series is defined as the fraction of t...

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Main Authors: Yahaya Z. Ibrahim, Heiko Balzter, Jörg Kaduk, Compton J. Tucker
Format: Article
Language:English
Published: MDPI AG 2015-04-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/7/5/5471
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author Yahaya Z. Ibrahim
Heiko Balzter
Jörg Kaduk
Compton J. Tucker
author_facet Yahaya Z. Ibrahim
Heiko Balzter
Jörg Kaduk
Compton J. Tucker
author_sort Yahaya Z. Ibrahim
collection DOAJ
description Areas affected by land degradation in Sub-Saharan West Africa between 1982 and 2012 are identified using time-series analysis of vegetation index data derived from satellites. The residual trend (RESTREND) of a Normalized Difference Vegetation Index (NDVI) time-series is defined as the fraction of the difference between the observed NDVI and the NDVI predicted from climate data. It has been widely used to study desertification and other forms of land degradation in drylands. The method works on the assumption that a negative trend of vegetation photosynthetic capacity is an indication of land degradation if it is independent from climate variability. In the past, many scientists depended on rainfall data as the major climatic factor controlling vegetation productivity in drylands when applying the RESTREND method. However, the water that is directly available to vegetation is stored as soil moisture, which is a function of cumulative rainfall, surface runoff, infiltration and evapotranspiration. In this study, the new NDVI third generation (NDVI3g), which was generated by the National Aeronautics and Space Administration-Goddard Space Flight Center Global Inventory Modeling and Mapping Studies (NASA-GSFC GIMMS) group, was used as a satellite-derived proxy of vegetation productivity, together with the soil moisture index product from the Climate Prediction Center (CPC) and rainfall data from the Climate Research Unit (CRU). The results show that the soil moisture/NDVI pixel-wise residual trend indicates land degraded areas more clearly than rainfall/NDVI. The spatial and temporal trends of the RESTREND in the region follow the patterns of drought episodes, reaffirming the difficulties in separating the impacts of drought and land degradation on vegetation photosynthetic capacity. Therefore, future studies of land degradation and desertification in drylands should go beyond using rainfall as a sole predictor of vegetation condition, and include soil moisture index datasets in the analysis.
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spelling doaj.art-de35610985564b71bb5e340b916d62bc2022-12-21T17:24:26ZengMDPI AGRemote Sensing2072-42922015-04-01755471549410.3390/rs70505471rs70505471Land Degradation Assessment Using Residual Trend Analysis of GIMMS NDVI3g, Soil Moisture and Rainfall in Sub-Saharan West Africa from 1982 to 2012Yahaya Z. Ibrahim0Heiko Balzter1Jörg Kaduk2Compton J. Tucker3Department of Geography, Centre for Landscape and Climate Research, University of Leicester, Leicester LE1 7RH, UKDepartment of Geography, Centre for Landscape and Climate Research, University of Leicester, Leicester LE1 7RH, UKDepartment of Geography, Centre for Landscape and Climate Research, University of Leicester, Leicester LE1 7RH, UKNASA Goddard Space Flight Centre, Mail Code 610.9, Greenbelt, MD 20771, USAAreas affected by land degradation in Sub-Saharan West Africa between 1982 and 2012 are identified using time-series analysis of vegetation index data derived from satellites. The residual trend (RESTREND) of a Normalized Difference Vegetation Index (NDVI) time-series is defined as the fraction of the difference between the observed NDVI and the NDVI predicted from climate data. It has been widely used to study desertification and other forms of land degradation in drylands. The method works on the assumption that a negative trend of vegetation photosynthetic capacity is an indication of land degradation if it is independent from climate variability. In the past, many scientists depended on rainfall data as the major climatic factor controlling vegetation productivity in drylands when applying the RESTREND method. However, the water that is directly available to vegetation is stored as soil moisture, which is a function of cumulative rainfall, surface runoff, infiltration and evapotranspiration. In this study, the new NDVI third generation (NDVI3g), which was generated by the National Aeronautics and Space Administration-Goddard Space Flight Center Global Inventory Modeling and Mapping Studies (NASA-GSFC GIMMS) group, was used as a satellite-derived proxy of vegetation productivity, together with the soil moisture index product from the Climate Prediction Center (CPC) and rainfall data from the Climate Research Unit (CRU). The results show that the soil moisture/NDVI pixel-wise residual trend indicates land degraded areas more clearly than rainfall/NDVI. The spatial and temporal trends of the RESTREND in the region follow the patterns of drought episodes, reaffirming the difficulties in separating the impacts of drought and land degradation on vegetation photosynthetic capacity. Therefore, future studies of land degradation and desertification in drylands should go beyond using rainfall as a sole predictor of vegetation condition, and include soil moisture index datasets in the analysis.http://www.mdpi.com/2072-4292/7/5/5471land degradationRESTRENDNDVI3gsoil moisturerainfallSub-Saharan West Africa
spellingShingle Yahaya Z. Ibrahim
Heiko Balzter
Jörg Kaduk
Compton J. Tucker
Land Degradation Assessment Using Residual Trend Analysis of GIMMS NDVI3g, Soil Moisture and Rainfall in Sub-Saharan West Africa from 1982 to 2012
Remote Sensing
land degradation
RESTREND
NDVI3g
soil moisture
rainfall
Sub-Saharan West Africa
title Land Degradation Assessment Using Residual Trend Analysis of GIMMS NDVI3g, Soil Moisture and Rainfall in Sub-Saharan West Africa from 1982 to 2012
title_full Land Degradation Assessment Using Residual Trend Analysis of GIMMS NDVI3g, Soil Moisture and Rainfall in Sub-Saharan West Africa from 1982 to 2012
title_fullStr Land Degradation Assessment Using Residual Trend Analysis of GIMMS NDVI3g, Soil Moisture and Rainfall in Sub-Saharan West Africa from 1982 to 2012
title_full_unstemmed Land Degradation Assessment Using Residual Trend Analysis of GIMMS NDVI3g, Soil Moisture and Rainfall in Sub-Saharan West Africa from 1982 to 2012
title_short Land Degradation Assessment Using Residual Trend Analysis of GIMMS NDVI3g, Soil Moisture and Rainfall in Sub-Saharan West Africa from 1982 to 2012
title_sort land degradation assessment using residual trend analysis of gimms ndvi3g soil moisture and rainfall in sub saharan west africa from 1982 to 2012
topic land degradation
RESTREND
NDVI3g
soil moisture
rainfall
Sub-Saharan West Africa
url http://www.mdpi.com/2072-4292/7/5/5471
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