Comparison between Vegetation and Rainfall of Bioclimatic Ecoregions in Central Africa

This paper investigates the relationship between the Normalized Difference Vegetation Index (NDVI) and extracted rainfall in the Global Precipitation Climatology Project (GPCP) in Central Africa between latitudes 15°S and 20°N and longitudes 0°E and 31°E. Monthly NDVI and GPCP datasets for the perio...

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Main Authors: Sonfack Rousvel, Nzeukou Armand, Lenouo Andre, Siddi Tengeleng, Tchakoutio Sandjon Alain, Kaptue Armel
Format: Article
Language:English
Published: MDPI AG 2013-11-01
Series:Atmosphere
Subjects:
Online Access:http://www.mdpi.com/2073-4433/4/4/411
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spelling doaj-dd5d8778c435452b9b26889c91f1c1a82020-11-25T00:57:54ZengMDPI AGAtmosphere2073-44332013-11-014441142710.3390/atmos4040411Comparison between Vegetation and Rainfall of Bioclimatic Ecoregions in Central AfricaSonfack RousvelNzeukou ArmandLenouo AndreSiddi TengelengTchakoutio Sandjon AlainKaptue ArmelThis paper investigates the relationship between the Normalized Difference Vegetation Index (NDVI) and extracted rainfall in the Global Precipitation Climatology Project (GPCP) in Central Africa between latitudes 15°S and 20°N and longitudes 0°E and 31°E. Monthly NDVI and GPCP datasets for the period 1982–2000 have been used. The Index of Segmentation of Fourier Components (ISFC) has been applied on the NDVI dataset to segment Central Africa into four bioclimatic ecoregions (BCERs). In order to compare the differential response of vegetation growth to rainfall, an analysis of the inter-annual, intra-annual and seasonal variability for each BCER has been carried out, and the correlations between NDVI and rainfall have been assessed. The plot of the annual cycles of both variables revealed a coherent onset, peak and decay, with a time lag of 1 month for almost all the zones, except the zones, semi-desert and steppe, where a season of short and intense rainfall was observed. The correlation coefficients computed between the two variables are relatively high, especially in brush-grass savannah, where they reach up to 0.90 at a time lag of 1 month. The phenological transition points and phases show that the range between the +1 and http://www.mdpi.com/2073-4433/4/4/411AVHRRGPCPISFCNDVIrainfallvegetation
collection DOAJ
language English
format Article
sources DOAJ
author Sonfack Rousvel
Nzeukou Armand
Lenouo Andre
Siddi Tengeleng
Tchakoutio Sandjon Alain
Kaptue Armel
spellingShingle Sonfack Rousvel
Nzeukou Armand
Lenouo Andre
Siddi Tengeleng
Tchakoutio Sandjon Alain
Kaptue Armel
Comparison between Vegetation and Rainfall of Bioclimatic Ecoregions in Central Africa
Atmosphere
AVHRR
GPCP
ISFC
NDVI
rainfall
vegetation
author_facet Sonfack Rousvel
Nzeukou Armand
Lenouo Andre
Siddi Tengeleng
Tchakoutio Sandjon Alain
Kaptue Armel
author_sort Sonfack Rousvel
title Comparison between Vegetation and Rainfall of Bioclimatic Ecoregions in Central Africa
title_short Comparison between Vegetation and Rainfall of Bioclimatic Ecoregions in Central Africa
title_full Comparison between Vegetation and Rainfall of Bioclimatic Ecoregions in Central Africa
title_fullStr Comparison between Vegetation and Rainfall of Bioclimatic Ecoregions in Central Africa
title_full_unstemmed Comparison between Vegetation and Rainfall of Bioclimatic Ecoregions in Central Africa
title_sort comparison between vegetation and rainfall of bioclimatic ecoregions in central africa
publisher MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2013-11-01
description This paper investigates the relationship between the Normalized Difference Vegetation Index (NDVI) and extracted rainfall in the Global Precipitation Climatology Project (GPCP) in Central Africa between latitudes 15°S and 20°N and longitudes 0°E and 31°E. Monthly NDVI and GPCP datasets for the period 1982–2000 have been used. The Index of Segmentation of Fourier Components (ISFC) has been applied on the NDVI dataset to segment Central Africa into four bioclimatic ecoregions (BCERs). In order to compare the differential response of vegetation growth to rainfall, an analysis of the inter-annual, intra-annual and seasonal variability for each BCER has been carried out, and the correlations between NDVI and rainfall have been assessed. The plot of the annual cycles of both variables revealed a coherent onset, peak and decay, with a time lag of 1 month for almost all the zones, except the zones, semi-desert and steppe, where a season of short and intense rainfall was observed. The correlation coefficients computed between the two variables are relatively high, especially in brush-grass savannah, where they reach up to 0.90 at a time lag of 1 month. The phenological transition points and phases show that the range between the +1 and
topic AVHRR
GPCP
ISFC
NDVI
rainfall
vegetation
url http://www.mdpi.com/2073-4433/4/4/411
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