Trends in Greenness and Snow Cover in Alaska’s Arctic National Parks, 2000–2016
In cold-limited arctic environments, the duration and timing of the snow cover and the vegetation green season have major ecological implications. I monitored the phenology of snow cover and greenness using MODIS Terra satellite data for the years 2000 to 2016 in the 5 National Parks of northern Ala...
Published in: | Remote Sensing |
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Main Author: | |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2017
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Subjects: | |
Online Access: | https://doi.org/10.3390/rs9060514 |
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author | David Swanson |
author_facet | David Swanson |
author_sort | David Swanson |
collection | MDPI Open Access Publishing |
container_issue | 6 |
container_start_page | 514 |
container_title | Remote Sensing |
container_volume | 9 |
description | In cold-limited arctic environments, the duration and timing of the snow cover and the vegetation green season have major ecological implications. I monitored the phenology of snow cover and greenness using MODIS Terra satellite data for the years 2000 to 2016 in the 5 National Parks of northern Alaska, USA. Mann-Kendall trend tests showed that the end of the continuous snow season and midpoint of spring green-up became significantly earlier in parts of the study area over the 16-year period. Using the observed relationship between thaw degree-days at Kotzebue, Alaska and dates of snow-off and half green-up in nearby lowland tundra for the 16 years of MODIS data, I reconstructed the dates of snow-off and half green-up from long-term Kotzebue weather records back to 1937. The average snow-off and green-up dates probably became earlier by about 6 days over this 80-year time interval. Remote sensing of fall vegetation senescence and establishment of the snow cover were less reliable than the spring events due to cloudiness and low sun angles. The annual maximum normalized difference vegetation index (NDVI) generally did not increase significantly from 2001 to 2016, except in places where vegetation was recovering from forest fires. |
format | Text |
genre | Arctic Tundra Alaska |
genre_facet | Arctic Tundra Alaska |
geographic | Arctic Kendall |
geographic_facet | Arctic Kendall |
id | ftmdpi:oai:mdpi.com:/2072-4292/9/6/514/ |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-59.828,-59.828,-63.497,-63.497) |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/rs9060514 |
op_relation | https://dx.doi.org/10.3390/rs9060514 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Remote Sensing; Volume 9; Issue 6; Pages: 514 |
publishDate | 2017 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/2072-4292/9/6/514/ 2025-01-16T20:22:34+00:00 Trends in Greenness and Snow Cover in Alaska’s Arctic National Parks, 2000–2016 David Swanson agris 2017-05-23 application/pdf https://doi.org/10.3390/rs9060514 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs9060514 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 9; Issue 6; Pages: 514 phenology greenness snow NDVI Alaska Arctic tundra Text 2017 ftmdpi https://doi.org/10.3390/rs9060514 2023-07-31T21:07:29Z In cold-limited arctic environments, the duration and timing of the snow cover and the vegetation green season have major ecological implications. I monitored the phenology of snow cover and greenness using MODIS Terra satellite data for the years 2000 to 2016 in the 5 National Parks of northern Alaska, USA. Mann-Kendall trend tests showed that the end of the continuous snow season and midpoint of spring green-up became significantly earlier in parts of the study area over the 16-year period. Using the observed relationship between thaw degree-days at Kotzebue, Alaska and dates of snow-off and half green-up in nearby lowland tundra for the 16 years of MODIS data, I reconstructed the dates of snow-off and half green-up from long-term Kotzebue weather records back to 1937. The average snow-off and green-up dates probably became earlier by about 6 days over this 80-year time interval. Remote sensing of fall vegetation senescence and establishment of the snow cover were less reliable than the spring events due to cloudiness and low sun angles. The annual maximum normalized difference vegetation index (NDVI) generally did not increase significantly from 2001 to 2016, except in places where vegetation was recovering from forest fires. Text Arctic Tundra Alaska MDPI Open Access Publishing Arctic Kendall ENVELOPE(-59.828,-59.828,-63.497,-63.497) Remote Sensing 9 6 514 |
spellingShingle | phenology greenness snow NDVI Alaska Arctic tundra David Swanson Trends in Greenness and Snow Cover in Alaska’s Arctic National Parks, 2000–2016 |
title | Trends in Greenness and Snow Cover in Alaska’s Arctic National Parks, 2000–2016 |
title_full | Trends in Greenness and Snow Cover in Alaska’s Arctic National Parks, 2000–2016 |
title_fullStr | Trends in Greenness and Snow Cover in Alaska’s Arctic National Parks, 2000–2016 |
title_full_unstemmed | Trends in Greenness and Snow Cover in Alaska’s Arctic National Parks, 2000–2016 |
title_short | Trends in Greenness and Snow Cover in Alaska’s Arctic National Parks, 2000–2016 |
title_sort | trends in greenness and snow cover in alaska’s arctic national parks, 2000–2016 |
topic | phenology greenness snow NDVI Alaska Arctic tundra |
topic_facet | phenology greenness snow NDVI Alaska Arctic tundra |
url | https://doi.org/10.3390/rs9060514 |