Vegetation phenology in Greenland and links to cryospheric change

Recent greening of vegetation across the Arctic is associated with warming temperatures, hydrologic change and shorter snow-covered periods. Here we investigated trends for a subset of arctic vegetation on the island of Greenland. Vegetation in Greenland is unique due to its close proximity to the G...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Jeffery A. Thompson, Lora S. Koenig
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2018
Subjects:
Online Access:https://doi.org/10.1017/aog.2018.24
https://doaj.org/article/89f6fc0f79234d6bbbdc3a5aa29dd032
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spelling ftdoajarticles:oai:doaj.org/article:89f6fc0f79234d6bbbdc3a5aa29dd032 2023-05-15T13:29:31+02:00 Vegetation phenology in Greenland and links to cryospheric change Jeffery A. Thompson Lora S. Koenig 2018-12-01T00:00:00Z https://doi.org/10.1017/aog.2018.24 https://doaj.org/article/89f6fc0f79234d6bbbdc3a5aa29dd032 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305518000241/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2018.24 0260-3055 1727-5644 https://doaj.org/article/89f6fc0f79234d6bbbdc3a5aa29dd032 Annals of Glaciology, Vol 59, Pp 59-68 (2018) Arctic warming Greenland land surface phenology MODIS seasonality Meteorology. Climatology QC851-999 article 2018 ftdoajarticles https://doi.org/10.1017/aog.2018.24 2023-03-12T01:31:57Z Recent greening of vegetation across the Arctic is associated with warming temperatures, hydrologic change and shorter snow-covered periods. Here we investigated trends for a subset of arctic vegetation on the island of Greenland. Vegetation in Greenland is unique due to its close proximity to the Greenland Ice Sheet and its proportionally large connection to the Greenlandic population through the hunting of grazing animals. The aim of this study was to determine whether or not longer snow-free periods (SFPs) were causing Greenlandic vegetation to dry out and become less productive. If vegetation was drying out, a subsequent aim of the study was to determine how widespread the drying was across Greenland. We utilized a 15-year time-series obtained by the MODerate Resolution Imaging Spectroradiometer (MODIS) to analyze the Greenland vegetation by deriving descriptors corresponding with the SFP, the number of cumulative growing degree-days and the time-integrated Normalized Difference Vegetation Index. While the productivity of most vegetated areas increased in response to longer growing periods, there were localized regions that exhibited signs consistent with the drying hypothesis. In these areas, vegetation productivity decreased in response to longer SFPs and more accumulated growing degree-days. Article in Journal/Newspaper Annals of Glaciology Arctic Greenland greenlandic Ice Sheet Directory of Open Access Journals: DOAJ Articles Arctic Greenland Annals of Glaciology 59 77 59 68
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic warming
Greenland
land surface phenology
MODIS
seasonality
Meteorology. Climatology
QC851-999
spellingShingle Arctic warming
Greenland
land surface phenology
MODIS
seasonality
Meteorology. Climatology
QC851-999
Jeffery A. Thompson
Lora S. Koenig
Vegetation phenology in Greenland and links to cryospheric change
topic_facet Arctic warming
Greenland
land surface phenology
MODIS
seasonality
Meteorology. Climatology
QC851-999
description Recent greening of vegetation across the Arctic is associated with warming temperatures, hydrologic change and shorter snow-covered periods. Here we investigated trends for a subset of arctic vegetation on the island of Greenland. Vegetation in Greenland is unique due to its close proximity to the Greenland Ice Sheet and its proportionally large connection to the Greenlandic population through the hunting of grazing animals. The aim of this study was to determine whether or not longer snow-free periods (SFPs) were causing Greenlandic vegetation to dry out and become less productive. If vegetation was drying out, a subsequent aim of the study was to determine how widespread the drying was across Greenland. We utilized a 15-year time-series obtained by the MODerate Resolution Imaging Spectroradiometer (MODIS) to analyze the Greenland vegetation by deriving descriptors corresponding with the SFP, the number of cumulative growing degree-days and the time-integrated Normalized Difference Vegetation Index. While the productivity of most vegetated areas increased in response to longer growing periods, there were localized regions that exhibited signs consistent with the drying hypothesis. In these areas, vegetation productivity decreased in response to longer SFPs and more accumulated growing degree-days.
format Article in Journal/Newspaper
author Jeffery A. Thompson
Lora S. Koenig
author_facet Jeffery A. Thompson
Lora S. Koenig
author_sort Jeffery A. Thompson
title Vegetation phenology in Greenland and links to cryospheric change
title_short Vegetation phenology in Greenland and links to cryospheric change
title_full Vegetation phenology in Greenland and links to cryospheric change
title_fullStr Vegetation phenology in Greenland and links to cryospheric change
title_full_unstemmed Vegetation phenology in Greenland and links to cryospheric change
title_sort vegetation phenology in greenland and links to cryospheric change
publisher Cambridge University Press
publishDate 2018
url https://doi.org/10.1017/aog.2018.24
https://doaj.org/article/89f6fc0f79234d6bbbdc3a5aa29dd032
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Annals of Glaciology
Arctic
Greenland
greenlandic
Ice Sheet
genre_facet Annals of Glaciology
Arctic
Greenland
greenlandic
Ice Sheet
op_source Annals of Glaciology, Vol 59, Pp 59-68 (2018)
op_relation https://www.cambridge.org/core/product/identifier/S0260305518000241/type/journal_article
https://doaj.org/toc/0260-3055
https://doaj.org/toc/1727-5644
doi:10.1017/aog.2018.24
0260-3055
1727-5644
https://doaj.org/article/89f6fc0f79234d6bbbdc3a5aa29dd032
op_doi https://doi.org/10.1017/aog.2018.24
container_title Annals of Glaciology
container_volume 59
container_issue 77
container_start_page 59
op_container_end_page 68
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