Vegetation dynamics and its relationship with climatic factors in the Changbai Mountain Natural Reserve

This study examined the temporal variation of the Normalized Difference Vegetation Index (NDVI) and its relationship with climatic factors in the Changbai Mountain Natural Reserve (CMNR) during 2000-2009. The results showed as follows. The average NDVI values increased at a rate of 0.0024 year-1. Th...

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Published in:Journal of Mountain Science
Main Authors: Hou, Guanglei, Zhang, Hongyan, Wang, Yeqiao
Format: Text
Language:unknown
Published: DigitalCommons@URI 2011
Subjects:
Online Access:https://digitalcommons.uri.edu/nrs_facpubs/871
https://doi.org/10.1007/s11629-011-2206-4
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spelling ftunivrhodeislan:oai:digitalcommons.uri.edu:nrs_facpubs-1872 2023-07-30T04:07:20+02:00 Vegetation dynamics and its relationship with climatic factors in the Changbai Mountain Natural Reserve Hou, Guanglei Zhang, Hongyan Wang, Yeqiao 2011-12-01T08:00:00Z https://digitalcommons.uri.edu/nrs_facpubs/871 https://doi.org/10.1007/s11629-011-2206-4 unknown DigitalCommons@URI https://digitalcommons.uri.edu/nrs_facpubs/871 doi:10.1007/s11629-011-2206-4 https://doi.org/10.1007/s11629-011-2206-4 Natural Resources Science Faculty Publications Changbai Mountain Natural Reserve Climatic factors Remote sensing SPOT/VGT NDVI text 2011 ftunivrhodeislan https://doi.org/10.1007/s11629-011-2206-4 2023-07-17T19:10:14Z This study examined the temporal variation of the Normalized Difference Vegetation Index (NDVI) and its relationship with climatic factors in the Changbai Mountain Natural Reserve (CMNR) during 2000-2009. The results showed as follows. The average NDVI values increased at a rate of 0.0024 year-1. The increase rate differed with vegetation types, such as 0.0034 year-1 for forest and 0.0017 year-1 for tundra. Trend analyses revealed a consistent NDVI increase at the start and end of the growing season but little variation or decrease observed in July during the study period. The NDVI in CMNR showed a stronger correlation with temperature than with precipitation, especially in spring and autumn. A stronger correlation was observed between NDVI and temperature in the tundra zone (2,000-2,600m) than in the coniferous forest (1,100-1,700m) and Korean pine-broadleaved mixed forest (700-1,100m) zones. The results indicate that vegetation at higher elevations is more sensitive to temperature change. NDVI variation had a strong correlation with temperature change (r=0.7311, p<0. 01) but less significant correlation with precipitation change. The result indicates that temperature can serve as a main indicator of vegetation sensitivity in the CMNR. © 2011 Science Press and Institute of Mountain Hazards and Environment, CAS and Springer-Verlag Berlin Heidelberg. Text Tundra University of Rhode Island: DigitalCommons@URI Journal of Mountain Science 8 6 865 875
institution Open Polar
collection University of Rhode Island: DigitalCommons@URI
op_collection_id ftunivrhodeislan
language unknown
topic Changbai Mountain Natural Reserve
Climatic factors
Remote sensing
SPOT/VGT NDVI
spellingShingle Changbai Mountain Natural Reserve
Climatic factors
Remote sensing
SPOT/VGT NDVI
Hou, Guanglei
Zhang, Hongyan
Wang, Yeqiao
Vegetation dynamics and its relationship with climatic factors in the Changbai Mountain Natural Reserve
topic_facet Changbai Mountain Natural Reserve
Climatic factors
Remote sensing
SPOT/VGT NDVI
description This study examined the temporal variation of the Normalized Difference Vegetation Index (NDVI) and its relationship with climatic factors in the Changbai Mountain Natural Reserve (CMNR) during 2000-2009. The results showed as follows. The average NDVI values increased at a rate of 0.0024 year-1. The increase rate differed with vegetation types, such as 0.0034 year-1 for forest and 0.0017 year-1 for tundra. Trend analyses revealed a consistent NDVI increase at the start and end of the growing season but little variation or decrease observed in July during the study period. The NDVI in CMNR showed a stronger correlation with temperature than with precipitation, especially in spring and autumn. A stronger correlation was observed between NDVI and temperature in the tundra zone (2,000-2,600m) than in the coniferous forest (1,100-1,700m) and Korean pine-broadleaved mixed forest (700-1,100m) zones. The results indicate that vegetation at higher elevations is more sensitive to temperature change. NDVI variation had a strong correlation with temperature change (r=0.7311, p<0. 01) but less significant correlation with precipitation change. The result indicates that temperature can serve as a main indicator of vegetation sensitivity in the CMNR. © 2011 Science Press and Institute of Mountain Hazards and Environment, CAS and Springer-Verlag Berlin Heidelberg.
format Text
author Hou, Guanglei
Zhang, Hongyan
Wang, Yeqiao
author_facet Hou, Guanglei
Zhang, Hongyan
Wang, Yeqiao
author_sort Hou, Guanglei
title Vegetation dynamics and its relationship with climatic factors in the Changbai Mountain Natural Reserve
title_short Vegetation dynamics and its relationship with climatic factors in the Changbai Mountain Natural Reserve
title_full Vegetation dynamics and its relationship with climatic factors in the Changbai Mountain Natural Reserve
title_fullStr Vegetation dynamics and its relationship with climatic factors in the Changbai Mountain Natural Reserve
title_full_unstemmed Vegetation dynamics and its relationship with climatic factors in the Changbai Mountain Natural Reserve
title_sort vegetation dynamics and its relationship with climatic factors in the changbai mountain natural reserve
publisher DigitalCommons@URI
publishDate 2011
url https://digitalcommons.uri.edu/nrs_facpubs/871
https://doi.org/10.1007/s11629-011-2206-4
genre Tundra
genre_facet Tundra
op_source Natural Resources Science Faculty Publications
op_relation https://digitalcommons.uri.edu/nrs_facpubs/871
doi:10.1007/s11629-011-2206-4
https://doi.org/10.1007/s11629-011-2206-4
op_doi https://doi.org/10.1007/s11629-011-2206-4
container_title Journal of Mountain Science
container_volume 8
container_issue 6
container_start_page 865
op_container_end_page 875
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