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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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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1766330789032624128 |