Trends in the Start of the Growing Season in Fennoscandia 1982–2011

Global temperature is increasing, and this is affecting the vegetation phenology in many parts of the world. In Fennoscandia, as well as Northern Europe, the advances of phenological events in spring have been recorded in recent decades. In this study, we analyzed the start of the growing season wit...

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Published in:Remote Sensing
Main Authors: Kjell Høgda, Hans Tømmervik, Stein Karlsen
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2013
Subjects:
Online Access:https://doi.org/10.3390/rs5094304
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author Kjell Høgda
Hans Tømmervik
Stein Karlsen
author_facet Kjell Høgda
Hans Tømmervik
Stein Karlsen
author_sort Kjell Høgda
collection MDPI Open Access Publishing
container_issue 9
container_start_page 4304
container_title Remote Sensing
container_volume 5
description Global temperature is increasing, and this is affecting the vegetation phenology in many parts of the world. In Fennoscandia, as well as Northern Europe, the advances of phenological events in spring have been recorded in recent decades. In this study, we analyzed the start of the growing season within five different vegetation regions in Fennoscandia using the 30-year Global Inventory Modeling and Mapping Studies (GIMMS) NDVI3g dataset. We applied a previously developed pixel-specific Normalized Difference Vegetation Index (NDVI) threshold method, adjusted it to the NDVI3g data and analyzed trends within the different regions. Results show a warming trend with an earlier start of the growing season of 11.8 ± 2.0 days (p < 0.01) for the whole area. However, there are large regional differences, and the warming/trend towards an earlier start of the growing season is most significant in the southern regions (19.3 ± 4.7 days, p < 0.01 in the southern oceanic region), while the start was stable or modest earlier (two to four days; not significant) in the northern regions. To look for temporal variations in the trends, we divided the 30-year period into three separate decadal time periods. Results show significantly more change/trend towards an earlier start of the growing season in the first period compared to the two last. In the second and third period, the trend towards an earlier start of the growing season slowed down, and in two of the regions, the trend towards an earlier start of the growing season was even reversed during the last decade.
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spelling ftmdpi:oai:mdpi.com:/2072-4292/5/9/4304/ 2025-01-16T21:50:20+00:00 Trends in the Start of the Growing Season in Fennoscandia 1982–2011 Kjell Høgda Hans Tømmervik Stein Karlsen agris 2013-09-06 application/pdf https://doi.org/10.3390/rs5094304 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs5094304 https://creativecommons.org/licenses/by/3.0/ Remote Sensing; Volume 5; Issue 9; Pages: 4304-4318 phenology start of the growing season NDVI time series NDVI3g Fennoscandia vegetation regions temporal trends Text 2013 ftmdpi https://doi.org/10.3390/rs5094304 2023-07-31T20:33:53Z Global temperature is increasing, and this is affecting the vegetation phenology in many parts of the world. In Fennoscandia, as well as Northern Europe, the advances of phenological events in spring have been recorded in recent decades. In this study, we analyzed the start of the growing season within five different vegetation regions in Fennoscandia using the 30-year Global Inventory Modeling and Mapping Studies (GIMMS) NDVI3g dataset. We applied a previously developed pixel-specific Normalized Difference Vegetation Index (NDVI) threshold method, adjusted it to the NDVI3g data and analyzed trends within the different regions. Results show a warming trend with an earlier start of the growing season of 11.8 ± 2.0 days (p < 0.01) for the whole area. However, there are large regional differences, and the warming/trend towards an earlier start of the growing season is most significant in the southern regions (19.3 ± 4.7 days, p < 0.01 in the southern oceanic region), while the start was stable or modest earlier (two to four days; not significant) in the northern regions. To look for temporal variations in the trends, we divided the 30-year period into three separate decadal time periods. Results show significantly more change/trend towards an earlier start of the growing season in the first period compared to the two last. In the second and third period, the trend towards an earlier start of the growing season slowed down, and in two of the regions, the trend towards an earlier start of the growing season was even reversed during the last decade. Text Fennoscandia MDPI Open Access Publishing Remote Sensing 5 9 4304 4318
spellingShingle phenology
start of the growing season
NDVI time series
NDVI3g
Fennoscandia
vegetation regions
temporal trends
Kjell Høgda
Hans Tømmervik
Stein Karlsen
Trends in the Start of the Growing Season in Fennoscandia 1982–2011
title Trends in the Start of the Growing Season in Fennoscandia 1982–2011
title_full Trends in the Start of the Growing Season in Fennoscandia 1982–2011
title_fullStr Trends in the Start of the Growing Season in Fennoscandia 1982–2011
title_full_unstemmed Trends in the Start of the Growing Season in Fennoscandia 1982–2011
title_short Trends in the Start of the Growing Season in Fennoscandia 1982–2011
title_sort trends in the start of the growing season in fennoscandia 1982–2011
topic phenology
start of the growing season
NDVI time series
NDVI3g
Fennoscandia
vegetation regions
temporal trends
topic_facet phenology
start of the growing season
NDVI time series
NDVI3g
Fennoscandia
vegetation regions
temporal trends
url https://doi.org/10.3390/rs5094304