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...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Author: David K. Swanson
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/rs13132554
id ftmdpi:oai:mdpi.com:/2072-4292/13/13/2554/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2072-4292/13/13/2554/ 2023-08-20T04:04:19+02:00 Start of the Green Season and Normalized Difference Vegetation Index in Alaska’s Arctic National Parks David K. Swanson agris 2021-06-30 application/pdf https://doi.org/10.3390/rs13132554 EN eng Multidisciplinary Digital Publishing Institute Remote Sensing in Agriculture and Vegetation https://dx.doi.org/10.3390/rs13132554 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 13; Issue 13; Pages: 2554 Alaska Arctic greenness NDVI phenology tundra Text 2021 ftmdpi https://doi.org/10.3390/rs13132554 2023-08-01T02:04:51Z 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. Text Arctic Tundra Alaska MDPI Open Access Publishing Arctic Remote Sensing 13 13 2554
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Alaska
Arctic
greenness
NDVI
phenology
tundra
spellingShingle Alaska
Arctic
greenness
NDVI
phenology
tundra
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
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 Text
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 Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/rs13132554
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
Tundra
Alaska
genre_facet Arctic
Tundra
Alaska
op_source Remote Sensing; Volume 13; Issue 13; Pages: 2554
op_relation Remote Sensing in Agriculture and Vegetation
https://dx.doi.org/10.3390/rs13132554
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs13132554
container_title Remote Sensing
container_volume 13
container_issue 13
container_start_page 2554
_version_ 1774714713814335488