Mapping and Attributing Normalized Difference Vegetation Index Trends for Nepal

Global change affects vegetation cover and processes through multiple pathways. Long time series of surface land surface properties derived from satellite remote sensing give unique abilities to observe these changes, particularly in areas with complex topography and limited research infrastructure....

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Main Authors: Nir Y. Krakauer, Tarendra Lakhankar, José D. Anadón
Format: Article
Language:English
Published: MDPI AG 2017-09-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/9/10/986
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spelling doaj-b2d4150ee04d4e1cbe62451105a538d72020-11-25T00:09:36ZengMDPI AGRemote Sensing2072-42922017-09-0191098610.3390/rs9100986rs9100986Mapping and Attributing Normalized Difference Vegetation Index Trends for NepalNir Y. Krakauer0Tarendra Lakhankar1José D. Anadón2Department of Civil Engineering and NOAA-CREST, City College of New York, New York, NY 10031, USADepartment of Civil Engineering and NOAA-CREST, City College of New York, New York, NY 10031, USAThe Graduate Center, City University of New York, New York, NY 10016, USAGlobal change affects vegetation cover and processes through multiple pathways. Long time series of surface land surface properties derived from satellite remote sensing give unique abilities to observe these changes, particularly in areas with complex topography and limited research infrastructure. Here, we focus on Nepal, a biodiversity hotspot where vegetation productivity is limited by moisture availability (dominated by a summer monsoon) at lower elevations and by temperature at high elevations. We analyze the normalized difference vegetation index (NDVI) from 1981 to 2015 semimonthly, at an 8 km spatial resolution. We use a random forest (RF) of regression trees to generate a statistical model of the NDVI as a function of elevation, land use, CO 2 level, temperature, and precipitation. We find that the NDVI increased over the studied period, particularly at low and middle elevations and during the fall (post-monsoon). We infer from the fitted RF model that the NDVI linear trend is primarily due to CO 2 level (or another environmental parameter that is changing quasi-linearly), and not primarily due to temperature or precipitation trends. On the other hand, interannual fluctuation in the NDVI is more correlated with temperature and precipitation. The RF accurately fits the available data and shows promise for estimating trends and testing hypotheses about their causes.https://www.mdpi.com/2072-4292/9/10/986random forestregression treecarbon fertilizationland cover changeclimate change
collection DOAJ
language English
format Article
sources DOAJ
author Nir Y. Krakauer
Tarendra Lakhankar
José D. Anadón
spellingShingle Nir Y. Krakauer
Tarendra Lakhankar
José D. Anadón
Mapping and Attributing Normalized Difference Vegetation Index Trends for Nepal
Remote Sensing
random forest
regression tree
carbon fertilization
land cover change
climate change
author_facet Nir Y. Krakauer
Tarendra Lakhankar
José D. Anadón
author_sort Nir Y. Krakauer
title Mapping and Attributing Normalized Difference Vegetation Index Trends for Nepal
title_short Mapping and Attributing Normalized Difference Vegetation Index Trends for Nepal
title_full Mapping and Attributing Normalized Difference Vegetation Index Trends for Nepal
title_fullStr Mapping and Attributing Normalized Difference Vegetation Index Trends for Nepal
title_full_unstemmed Mapping and Attributing Normalized Difference Vegetation Index Trends for Nepal
title_sort mapping and attributing normalized difference vegetation index trends for nepal
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2017-09-01
description Global change affects vegetation cover and processes through multiple pathways. Long time series of surface land surface properties derived from satellite remote sensing give unique abilities to observe these changes, particularly in areas with complex topography and limited research infrastructure. Here, we focus on Nepal, a biodiversity hotspot where vegetation productivity is limited by moisture availability (dominated by a summer monsoon) at lower elevations and by temperature at high elevations. We analyze the normalized difference vegetation index (NDVI) from 1981 to 2015 semimonthly, at an 8 km spatial resolution. We use a random forest (RF) of regression trees to generate a statistical model of the NDVI as a function of elevation, land use, CO 2 level, temperature, and precipitation. We find that the NDVI increased over the studied period, particularly at low and middle elevations and during the fall (post-monsoon). We infer from the fitted RF model that the NDVI linear trend is primarily due to CO 2 level (or another environmental parameter that is changing quasi-linearly), and not primarily due to temperature or precipitation trends. On the other hand, interannual fluctuation in the NDVI is more correlated with temperature and precipitation. The RF accurately fits the available data and shows promise for estimating trends and testing hypotheses about their causes.
topic random forest
regression tree
carbon fertilization
land cover change
climate change
url https://www.mdpi.com/2072-4292/9/10/986
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