Local variation in mountain birch spring phenology along an altitudinal gradient in northern coastal Fennoscandia

Currently there is a lack of spring phenology studies covering small-scale altitudinal gradients of mountain birch in coastal northern Fennoscandia, a region characterized by exceptionally high precipitation of snow, which gives reason to investigate the influence of snow cover on birch budburst in...

Full description

Bibliographic Details
Main Author: Sjöskog, Maja Sofia
Format: Master Thesis
Language:English
Published: Universitetet i Tromsø 2011
Subjects:
Online Access:https://hdl.handle.net/10037/3651
id ftunivtroemsoe:oai:munin.uit.no:10037/3651
record_format openpolar
spelling ftunivtroemsoe:oai:munin.uit.no:10037/3651 2023-05-15T16:11:45+02:00 Local variation in mountain birch spring phenology along an altitudinal gradient in northern coastal Fennoscandia Sjöskog, Maja Sofia 2011-06-10 https://hdl.handle.net/10037/3651 eng eng Universitetet i Tromsø University of Tromsø https://hdl.handle.net/10037/3651 URN:NBN:no-uit_munin_3367 openAccess Copyright 2011 The Author(s) VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ecology: 488 BIO-3910 Master thesis Mastergradsoppgave 2011 ftunivtroemsoe 2021-06-25T17:53:08Z Currently there is a lack of spring phenology studies covering small-scale altitudinal gradients of mountain birch in coastal northern Fennoscandia, a region characterized by exceptionally high precipitation of snow, which gives reason to investigate the influence of snow cover on birch budburst in this area. Furthermore, ground phenology studies are today increasingly replaced by satellite data studies, but only too rarely is the latter approach properly validated. In order to provide a better basis for studies of local variation in spring phenology of birch in coastal altitudinal gradients, this study aimed at exploring how well (1) thermal sum models could predict budburst in individual birch trees with the inclusion of local conditions such as snow depth, soil temperature and altitude as predictors, and (2) NDVI values from high-resolution satellite images reflect leaf phenology in birch. The result for (1) showed that a simple thermal time model with spring air temperatures provided the best explanation for budburst, and that snow depth, soil temperature and altitude did not improve the predictions. The results for (2) showed that the correspondence between NDVI values and leaf phenology was generally high, but there were still some variation between in situ measurements and the satellite-derived NDVI, probably reflecting the limited capacity of satellite imagery to capture the phenology of merely one species. Master Thesis Fennoscandia University of Tromsø: Munin Open Research Archive
institution Open Polar
collection University of Tromsø: Munin Open Research Archive
op_collection_id ftunivtroemsoe
language English
topic VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ecology: 488
BIO-3910
spellingShingle VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ecology: 488
BIO-3910
Sjöskog, Maja Sofia
Local variation in mountain birch spring phenology along an altitudinal gradient in northern coastal Fennoscandia
topic_facet VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ecology: 488
BIO-3910
description Currently there is a lack of spring phenology studies covering small-scale altitudinal gradients of mountain birch in coastal northern Fennoscandia, a region characterized by exceptionally high precipitation of snow, which gives reason to investigate the influence of snow cover on birch budburst in this area. Furthermore, ground phenology studies are today increasingly replaced by satellite data studies, but only too rarely is the latter approach properly validated. In order to provide a better basis for studies of local variation in spring phenology of birch in coastal altitudinal gradients, this study aimed at exploring how well (1) thermal sum models could predict budburst in individual birch trees with the inclusion of local conditions such as snow depth, soil temperature and altitude as predictors, and (2) NDVI values from high-resolution satellite images reflect leaf phenology in birch. The result for (1) showed that a simple thermal time model with spring air temperatures provided the best explanation for budburst, and that snow depth, soil temperature and altitude did not improve the predictions. The results for (2) showed that the correspondence between NDVI values and leaf phenology was generally high, but there were still some variation between in situ measurements and the satellite-derived NDVI, probably reflecting the limited capacity of satellite imagery to capture the phenology of merely one species.
format Master Thesis
author Sjöskog, Maja Sofia
author_facet Sjöskog, Maja Sofia
author_sort Sjöskog, Maja Sofia
title Local variation in mountain birch spring phenology along an altitudinal gradient in northern coastal Fennoscandia
title_short Local variation in mountain birch spring phenology along an altitudinal gradient in northern coastal Fennoscandia
title_full Local variation in mountain birch spring phenology along an altitudinal gradient in northern coastal Fennoscandia
title_fullStr Local variation in mountain birch spring phenology along an altitudinal gradient in northern coastal Fennoscandia
title_full_unstemmed Local variation in mountain birch spring phenology along an altitudinal gradient in northern coastal Fennoscandia
title_sort local variation in mountain birch spring phenology along an altitudinal gradient in northern coastal fennoscandia
publisher Universitetet i Tromsø
publishDate 2011
url https://hdl.handle.net/10037/3651
genre Fennoscandia
genre_facet Fennoscandia
op_relation https://hdl.handle.net/10037/3651
URN:NBN:no-uit_munin_3367
op_rights openAccess
Copyright 2011 The Author(s)
_version_ 1765996919199367168