Start of the Green Season and Normalized Difference Vegetation Index in Alaska’s Arctic National Parks

Daily Normalized Difference Vegetation Index (NDVI) values from the MODIS Aqua and Terra satellites were compared with on-the-ground camera observations at five locations in northern Alaska. Over half of the spring rise in NDVI was due to the transition from the snow-covered landscape to the snow-fr...

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Published in:Remote Sensing
Main Author: David K. Swanson
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Q
Online Access:https://doi.org/10.3390/rs13132554
https://doaj.org/article/bb0e06b738834d84832360d499757d5d
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spelling ftdoajarticles:oai:doaj.org/article:bb0e06b738834d84832360d499757d5d 2023-05-15T14:58:40+02:00 Start of the Green Season and Normalized Difference Vegetation Index in Alaska’s Arctic National Parks David K. Swanson 2021-06-01T00:00:00Z https://doi.org/10.3390/rs13132554 https://doaj.org/article/bb0e06b738834d84832360d499757d5d EN eng MDPI AG https://www.mdpi.com/2072-4292/13/13/2554 https://doaj.org/toc/2072-4292 doi:10.3390/rs13132554 2072-4292 https://doaj.org/article/bb0e06b738834d84832360d499757d5d Remote Sensing, Vol 13, Iss 2554, p 2554 (2021) Alaska Arctic greenness NDVI phenology tundra Science Q article 2021 ftdoajarticles https://doi.org/10.3390/rs13132554 2022-12-30T20:18:47Z Daily Normalized Difference Vegetation Index (NDVI) values from the MODIS Aqua and Terra satellites were compared with on-the-ground camera observations at five locations in northern Alaska. Over half of the spring rise in NDVI was due to the transition from the snow-covered landscape to the snow-free surface prior to the deciduous leaf-out. In the fall after the green season, NDVI fluctuated between an intermediate level representing senesced vegetation and lower values representing clouds and intermittent snow, and then dropped to constant low levels after establishment of the permanent winter snow cover. The NDVI value of snow-free surfaces after fall leaf senescence was estimated from multi-year data using a 90th percentile smoothing spline curve fit to a plot of daily NDVI values vs. ordinal date. This curve typically showed a flat region of intermediate NDVI values in the fall that represent cloud- and snow-free days with senesced vegetation. This “fall plateau” was readily identified in a large systematic sample of MODIS NDVI values across the study area, in typical tundra, shrub, and boreal forest environments. The NDVI level of the fall plateau can be extrapolated to the spring rising leg of the annual NDVI curve to approximate the true start of green season. Article in Journal/Newspaper Arctic Tundra Alaska Directory of Open Access Journals: DOAJ Articles Arctic Remote Sensing 13 13 2554
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Alaska
Arctic
greenness
NDVI
phenology
tundra
Science
Q
spellingShingle Alaska
Arctic
greenness
NDVI
phenology
tundra
Science
Q
David K. Swanson
Start of the Green Season and Normalized Difference Vegetation Index in Alaska’s Arctic National Parks
topic_facet Alaska
Arctic
greenness
NDVI
phenology
tundra
Science
Q
description Daily Normalized Difference Vegetation Index (NDVI) values from the MODIS Aqua and Terra satellites were compared with on-the-ground camera observations at five locations in northern Alaska. Over half of the spring rise in NDVI was due to the transition from the snow-covered landscape to the snow-free surface prior to the deciduous leaf-out. In the fall after the green season, NDVI fluctuated between an intermediate level representing senesced vegetation and lower values representing clouds and intermittent snow, and then dropped to constant low levels after establishment of the permanent winter snow cover. The NDVI value of snow-free surfaces after fall leaf senescence was estimated from multi-year data using a 90th percentile smoothing spline curve fit to a plot of daily NDVI values vs. ordinal date. This curve typically showed a flat region of intermediate NDVI values in the fall that represent cloud- and snow-free days with senesced vegetation. This “fall plateau” was readily identified in a large systematic sample of MODIS NDVI values across the study area, in typical tundra, shrub, and boreal forest environments. The NDVI level of the fall plateau can be extrapolated to the spring rising leg of the annual NDVI curve to approximate the true start of green season.
format Article in Journal/Newspaper
author David K. Swanson
author_facet David K. Swanson
author_sort David K. Swanson
title Start of the Green Season and Normalized Difference Vegetation Index in Alaska’s Arctic National Parks
title_short Start of the Green Season and Normalized Difference Vegetation Index in Alaska’s Arctic National Parks
title_full Start of the Green Season and Normalized Difference Vegetation Index in Alaska’s Arctic National Parks
title_fullStr Start of the Green Season and Normalized Difference Vegetation Index in Alaska’s Arctic National Parks
title_full_unstemmed Start of the Green Season and Normalized Difference Vegetation Index in Alaska’s Arctic National Parks
title_sort start of the green season and normalized difference vegetation index in alaska’s arctic national parks
publisher MDPI AG
publishDate 2021
url https://doi.org/10.3390/rs13132554
https://doaj.org/article/bb0e06b738834d84832360d499757d5d
geographic Arctic
geographic_facet Arctic
genre Arctic
Tundra
Alaska
genre_facet Arctic
Tundra
Alaska
op_source Remote Sensing, Vol 13, Iss 2554, p 2554 (2021)
op_relation https://www.mdpi.com/2072-4292/13/13/2554
https://doaj.org/toc/2072-4292
doi:10.3390/rs13132554
2072-4292
https://doaj.org/article/bb0e06b738834d84832360d499757d5d
op_doi https://doi.org/10.3390/rs13132554
container_title Remote Sensing
container_volume 13
container_issue 13
container_start_page 2554
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