Spatial and Temporal Variation of Drought Based on Satellite Derived Vegetation Condition Index in Nepal from 1982–2015

Identification of drought is essential for many environmental and agricultural applications. To further understand drought, this study presented spatial and temporal variations of drought based on satellite derived Vegetation Condition Index (VCI) on annual (Jan⁻Dec), seasonal monsoon (Jun...

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Main Authors: Binod Baniya, Qiuhong Tang, Ximeng Xu, Gebremedhin Gebremeskel Haile, Gyan Chhipi-Shrestha
Format: Article
Language:English
Published: MDPI AG 2019-01-01
Series:Sensors
Subjects:
Online Access:https://www.mdpi.com/1424-8220/19/2/430
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author Binod Baniya
Qiuhong Tang
Ximeng Xu
Gebremedhin Gebremeskel Haile
Gyan Chhipi-Shrestha
author_facet Binod Baniya
Qiuhong Tang
Ximeng Xu
Gebremedhin Gebremeskel Haile
Gyan Chhipi-Shrestha
author_sort Binod Baniya
collection DOAJ
description Identification of drought is essential for many environmental and agricultural applications. To further understand drought, this study presented spatial and temporal variations of drought based on satellite derived Vegetation Condition Index (VCI) on annual (Jan&#8315;Dec), seasonal monsoon (Jun&#8315;Nov) and pre-monsoon (Mar&#8315;May) scales from 1982&#8315;2015 in Nepal. The Vegetation Condition Index (VCI) obtained from NOAA, AVHRR (National Oceanic and Atmospheric Administration, Advanced Very High Resolution Radiometer) and climate data from meteorological stations were used. VCI was used to grade the drought, and the Mann&#8315;Kendall test and linear trend analysis were conducted to examine drought trends and the Pearson correlation between VCI and climatic factors (i.e., temperature and precipitation) was also acquired. The results identified that severe drought was identified in 1982, 1984, 1985 and 2000 on all time scales. However, VCI has increased at the rate of 1.14 yr<sup>&#8722;1</sup> (<i>p</i> = 0.04), 1.31 yr<sup>&#8722;1</sup> (<i>p</i> = 0.03) and 0.77 yr<sup>&#8722;1</sup> (<i>p</i> = 0.77) on the annual, seasonal monsoon and pre-monsoon scales, respectively. These increased VCIs indicated decreases in drought. However, spatially, increased trends of drought were also found in some regions in Nepal. For instance, northern areas mainly in the Trans-Himalayan regions identified severe drought. The foothills and the lowlands of Terai (southern Nepal) experienced normal VCI, i.e., no drought. Similarly, the Anomaly Vegetation Condition Index (AVCI) was mostly negative before 2000 which indicated deficient soil moisture. The exceedance probability analysis results on the annual time scale showed that there was a 20% chance of occurring severe drought (VCI &#8804; 35%) and a 35% chance of occurring normal drought (35% &#8804; VCI &#8804; 50%) in Nepal. Drought was also linked with climates in which temperature on the annual and seasonal monsoon scales was significant and positively correlated with VCI. Drought occurrence and trends in Nepal need to be further studied for comprehensive information and understanding.
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spelling doaj.art-f3a3a372c9c7454c829526b22d83f5912022-12-22T03:45:29ZengMDPI AGSensors1424-82202019-01-0119243010.3390/s19020430s19020430Spatial and Temporal Variation of Drought Based on Satellite Derived Vegetation Condition Index in Nepal from 1982–2015Binod Baniya0Qiuhong Tang1Ximeng Xu2Gebremedhin Gebremeskel Haile3Gyan Chhipi-Shrestha4Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, ChinaKey Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, ChinaKey Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, ChinaKey Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, ChinaÉcole Supérieure d’Amenagement du Territoire, Université Laval, 1628 Pavillon Savard, Université Laval, Québec City, QC G1K7P4, CanadaIdentification of drought is essential for many environmental and agricultural applications. To further understand drought, this study presented spatial and temporal variations of drought based on satellite derived Vegetation Condition Index (VCI) on annual (Jan&#8315;Dec), seasonal monsoon (Jun&#8315;Nov) and pre-monsoon (Mar&#8315;May) scales from 1982&#8315;2015 in Nepal. The Vegetation Condition Index (VCI) obtained from NOAA, AVHRR (National Oceanic and Atmospheric Administration, Advanced Very High Resolution Radiometer) and climate data from meteorological stations were used. VCI was used to grade the drought, and the Mann&#8315;Kendall test and linear trend analysis were conducted to examine drought trends and the Pearson correlation between VCI and climatic factors (i.e., temperature and precipitation) was also acquired. The results identified that severe drought was identified in 1982, 1984, 1985 and 2000 on all time scales. However, VCI has increased at the rate of 1.14 yr<sup>&#8722;1</sup> (<i>p</i> = 0.04), 1.31 yr<sup>&#8722;1</sup> (<i>p</i> = 0.03) and 0.77 yr<sup>&#8722;1</sup> (<i>p</i> = 0.77) on the annual, seasonal monsoon and pre-monsoon scales, respectively. These increased VCIs indicated decreases in drought. However, spatially, increased trends of drought were also found in some regions in Nepal. For instance, northern areas mainly in the Trans-Himalayan regions identified severe drought. The foothills and the lowlands of Terai (southern Nepal) experienced normal VCI, i.e., no drought. Similarly, the Anomaly Vegetation Condition Index (AVCI) was mostly negative before 2000 which indicated deficient soil moisture. The exceedance probability analysis results on the annual time scale showed that there was a 20% chance of occurring severe drought (VCI &#8804; 35%) and a 35% chance of occurring normal drought (35% &#8804; VCI &#8804; 50%) in Nepal. Drought was also linked with climates in which temperature on the annual and seasonal monsoon scales was significant and positively correlated with VCI. Drought occurrence and trends in Nepal need to be further studied for comprehensive information and understanding.https://www.mdpi.com/1424-8220/19/2/430VCIdroughtexceedance probabilityclimateNepal
spellingShingle Binod Baniya
Qiuhong Tang
Ximeng Xu
Gebremedhin Gebremeskel Haile
Gyan Chhipi-Shrestha
Spatial and Temporal Variation of Drought Based on Satellite Derived Vegetation Condition Index in Nepal from 1982–2015
Sensors
VCI
drought
exceedance probability
climate
Nepal
title Spatial and Temporal Variation of Drought Based on Satellite Derived Vegetation Condition Index in Nepal from 1982–2015
title_full Spatial and Temporal Variation of Drought Based on Satellite Derived Vegetation Condition Index in Nepal from 1982–2015
title_fullStr Spatial and Temporal Variation of Drought Based on Satellite Derived Vegetation Condition Index in Nepal from 1982–2015
title_full_unstemmed Spatial and Temporal Variation of Drought Based on Satellite Derived Vegetation Condition Index in Nepal from 1982–2015
title_short Spatial and Temporal Variation of Drought Based on Satellite Derived Vegetation Condition Index in Nepal from 1982–2015
title_sort spatial and temporal variation of drought based on satellite derived vegetation condition index in nepal from 1982 2015
topic VCI
drought
exceedance probability
climate
Nepal
url https://www.mdpi.com/1424-8220/19/2/430
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AT qiuhongtang spatialandtemporalvariationofdroughtbasedonsatellitederivedvegetationconditionindexinnepalfrom19822015
AT ximengxu spatialandtemporalvariationofdroughtbasedonsatellitederivedvegetationconditionindexinnepalfrom19822015
AT gebremedhingebremeskelhaile spatialandtemporalvariationofdroughtbasedonsatellitederivedvegetationconditionindexinnepalfrom19822015
AT gyanchhipishrestha spatialandtemporalvariationofdroughtbasedonsatellitederivedvegetationconditionindexinnepalfrom19822015