Global Trends in Seasonality of Normalized Difference Vegetation Index (NDVI), 1982–2011

A 30-year series of global monthly Normalized Difference Vegetation Index (NDVI) imagery derived from the Global Inventory Modeling and Mapping Studies (GIMMS) NDVI3g archive was analyzed for the presence of trends in changing seasonality. Using the Seasonal Trend Analysis (STA) procedure, over half...

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Published in:Remote Sensing
Main Authors: J. Eastman, Florencia Sangermano, Elia Machado, John Rogan, Assaf Anyamba
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2013
Subjects:
Online Access:https://doi.org/10.3390/rs5104799
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spelling ftmdpi:oai:mdpi.com:/2072-4292/5/10/4799/ 2023-08-20T04:10:06+02:00 Global Trends in Seasonality of Normalized Difference Vegetation Index (NDVI), 1982–2011 J. Eastman Florencia Sangermano Elia Machado John Rogan Assaf Anyamba agris 2013-09-30 application/pdf https://doi.org/10.3390/rs5104799 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs5104799 https://creativecommons.org/licenses/by/3.0/ Remote Sensing; Volume 5; Issue 10; Pages: 4799-4818 NDVI GIMMS NDVI3g Seasonal Trend Analysis AVHRR phenology Text 2013 ftmdpi https://doi.org/10.3390/rs5104799 2023-07-31T20:34:11Z A 30-year series of global monthly Normalized Difference Vegetation Index (NDVI) imagery derived from the Global Inventory Modeling and Mapping Studies (GIMMS) NDVI3g archive was analyzed for the presence of trends in changing seasonality. Using the Seasonal Trend Analysis (STA) procedure, over half (56.30%) of land surfaces were found to exhibit significant trends. Almost half (46.10%) of the significant trends belonged to three classes of seasonal trends (or changes). Class 1 consisted of areas that experienced a uniform increase in NDVI throughout the year, and was primarily associated with forested areas, particularly broadleaf forests. Class 2 consisted of areas experiencing an increase in the amplitude of the annual seasonal signal whereby increases in NDVI in the green season were balanced by decreases in the brown season. These areas were found primarily in grassland and shrubland regions. Class 3 was found primarily in the Taiga and Tundra biomes and exhibited increases in the annual summer peak in NDVI. While no single attribution of cause could be determined for each of these classes, it was evident that they are primarily found in natural areas (as opposed to anthropogenic land cover conversions) and that they are consistent with climate-related ameliorations of growing conditions during the study period. Text taiga Tundra MDPI Open Access Publishing Remote Sensing 5 10 4799 4818
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic NDVI
GIMMS NDVI3g
Seasonal Trend Analysis
AVHRR
phenology
spellingShingle NDVI
GIMMS NDVI3g
Seasonal Trend Analysis
AVHRR
phenology
J. Eastman
Florencia Sangermano
Elia Machado
John Rogan
Assaf Anyamba
Global Trends in Seasonality of Normalized Difference Vegetation Index (NDVI), 1982–2011
topic_facet NDVI
GIMMS NDVI3g
Seasonal Trend Analysis
AVHRR
phenology
description A 30-year series of global monthly Normalized Difference Vegetation Index (NDVI) imagery derived from the Global Inventory Modeling and Mapping Studies (GIMMS) NDVI3g archive was analyzed for the presence of trends in changing seasonality. Using the Seasonal Trend Analysis (STA) procedure, over half (56.30%) of land surfaces were found to exhibit significant trends. Almost half (46.10%) of the significant trends belonged to three classes of seasonal trends (or changes). Class 1 consisted of areas that experienced a uniform increase in NDVI throughout the year, and was primarily associated with forested areas, particularly broadleaf forests. Class 2 consisted of areas experiencing an increase in the amplitude of the annual seasonal signal whereby increases in NDVI in the green season were balanced by decreases in the brown season. These areas were found primarily in grassland and shrubland regions. Class 3 was found primarily in the Taiga and Tundra biomes and exhibited increases in the annual summer peak in NDVI. While no single attribution of cause could be determined for each of these classes, it was evident that they are primarily found in natural areas (as opposed to anthropogenic land cover conversions) and that they are consistent with climate-related ameliorations of growing conditions during the study period.
format Text
author J. Eastman
Florencia Sangermano
Elia Machado
John Rogan
Assaf Anyamba
author_facet J. Eastman
Florencia Sangermano
Elia Machado
John Rogan
Assaf Anyamba
author_sort J. Eastman
title Global Trends in Seasonality of Normalized Difference Vegetation Index (NDVI), 1982–2011
title_short Global Trends in Seasonality of Normalized Difference Vegetation Index (NDVI), 1982–2011
title_full Global Trends in Seasonality of Normalized Difference Vegetation Index (NDVI), 1982–2011
title_fullStr Global Trends in Seasonality of Normalized Difference Vegetation Index (NDVI), 1982–2011
title_full_unstemmed Global Trends in Seasonality of Normalized Difference Vegetation Index (NDVI), 1982–2011
title_sort global trends in seasonality of normalized difference vegetation index (ndvi), 1982–2011
publisher Multidisciplinary Digital Publishing Institute
publishDate 2013
url https://doi.org/10.3390/rs5104799
op_coverage agris
genre taiga
Tundra
genre_facet taiga
Tundra
op_source Remote Sensing; Volume 5; Issue 10; Pages: 4799-4818
op_relation https://dx.doi.org/10.3390/rs5104799
op_rights https://creativecommons.org/licenses/by/3.0/
op_doi https://doi.org/10.3390/rs5104799
container_title Remote Sensing
container_volume 5
container_issue 10
container_start_page 4799
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