Warming, Sheep and Volcanoes: Land Cover Changes in Iceland Evident in Satellite NDVI Trends

In a greening Arctic, Iceland stands out as an area with very high increases in the AVHRR Normalized Difference Vegetation Index (NDVI, 1982–2010). We investigated the possible sources of this anomalous greening in Iceland’s dynamic landscape, analyzing changes due to volcanism and warming temperatu...

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Main Authors: Martha Raynolds, Borgþór Magnússon, Sigmar Metúsalemsson, Sigurður H. Magnússon
Format: Article
Language:English
Published: MDPI AG 2015-07-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/7/8/9492
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author Martha Raynolds
Borgþór Magnússon
Sigmar Metúsalemsson
Sigurður H. Magnússon
author_facet Martha Raynolds
Borgþór Magnússon
Sigmar Metúsalemsson
Sigurður H. Magnússon
author_sort Martha Raynolds
collection DOAJ
description In a greening Arctic, Iceland stands out as an area with very high increases in the AVHRR Normalized Difference Vegetation Index (NDVI, 1982–2010). We investigated the possible sources of this anomalous greening in Iceland’s dynamic landscape, analyzing changes due to volcanism and warming temperatures, and the effects of agricultural and industrial land use changes. The analysis showed the increases were likely due to reductions in grazing in erosion-prone rangelands, extensive reclamation and afforestation efforts, as well as a response to warming climate, including glacial retreat. Like Scandinavia and much of the rest of the Arctic, Iceland has shown a recent reduction in NDVI since 2002, but still above pre-2000 levels. Theil-Sen robust regression analysis of MODIS NDVI trends from 2002 to 2013 showed Iceland had a slightly negative NDVI trend of 0.003 NDVI units/year (p < 0.05), with significant decreases in an area three times greater (29,809 km2) than that with increases (9419 km2). Specific areas with large decreases in NDVI during the last decade were due to the formation of a large reservoir as a part of a hydroelectric power project (Kárahnjúkar, 2002–2009), and due to ashfall from two volcanic eruptions (Eyjafjallajökull, 2010; Grímsvötn, 2011). Increases in NDVI in the last decade were found in erosion control areas, around retreating glaciers, and in other areas of plant colonization following natural disturbance. Our analysis demonstrates the effectiveness of MODIS NDVI for identifying the causes of changes in land cover, and confirms the reduction in NDVI in the last decade using both the AVHRR and MODIS satellite data.
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spelling doaj.art-b5b7f42a76c04a7c875e20aaf84c3ec32022-12-21T17:17:28ZengMDPI AGRemote Sensing2072-42922015-07-01789492950610.3390/rs70809492rs70809492Warming, Sheep and Volcanoes: Land Cover Changes in Iceland Evident in Satellite NDVI TrendsMartha Raynolds0Borgþór Magnússon1Sigmar Metúsalemsson2Sigurður H. Magnússon3Institute of Arctic Biology, University of Alaska Fairbanks, PO Box 757000, Fairbanks AK 99775, USAIcelandic Institute of Natural History, PO Box 125, 212 Garðabær, IcelandIcelandic Institute of Natural History, PO Box 125, 212 Garðabær, IcelandIcelandic Institute of Natural History, PO Box 125, 212 Garðabær, IcelandIn a greening Arctic, Iceland stands out as an area with very high increases in the AVHRR Normalized Difference Vegetation Index (NDVI, 1982–2010). We investigated the possible sources of this anomalous greening in Iceland’s dynamic landscape, analyzing changes due to volcanism and warming temperatures, and the effects of agricultural and industrial land use changes. The analysis showed the increases were likely due to reductions in grazing in erosion-prone rangelands, extensive reclamation and afforestation efforts, as well as a response to warming climate, including glacial retreat. Like Scandinavia and much of the rest of the Arctic, Iceland has shown a recent reduction in NDVI since 2002, but still above pre-2000 levels. Theil-Sen robust regression analysis of MODIS NDVI trends from 2002 to 2013 showed Iceland had a slightly negative NDVI trend of 0.003 NDVI units/year (p < 0.05), with significant decreases in an area three times greater (29,809 km2) than that with increases (9419 km2). Specific areas with large decreases in NDVI during the last decade were due to the formation of a large reservoir as a part of a hydroelectric power project (Kárahnjúkar, 2002–2009), and due to ashfall from two volcanic eruptions (Eyjafjallajökull, 2010; Grímsvötn, 2011). Increases in NDVI in the last decade were found in erosion control areas, around retreating glaciers, and in other areas of plant colonization following natural disturbance. Our analysis demonstrates the effectiveness of MODIS NDVI for identifying the causes of changes in land cover, and confirms the reduction in NDVI in the last decade using both the AVHRR and MODIS satellite data.http://www.mdpi.com/2072-4292/7/8/9492AHVRRMODISland coverland useNDVI
spellingShingle Martha Raynolds
Borgþór Magnússon
Sigmar Metúsalemsson
Sigurður H. Magnússon
Warming, Sheep and Volcanoes: Land Cover Changes in Iceland Evident in Satellite NDVI Trends
Remote Sensing
AHVRR
MODIS
land cover
land use
NDVI
title Warming, Sheep and Volcanoes: Land Cover Changes in Iceland Evident in Satellite NDVI Trends
title_full Warming, Sheep and Volcanoes: Land Cover Changes in Iceland Evident in Satellite NDVI Trends
title_fullStr Warming, Sheep and Volcanoes: Land Cover Changes in Iceland Evident in Satellite NDVI Trends
title_full_unstemmed Warming, Sheep and Volcanoes: Land Cover Changes in Iceland Evident in Satellite NDVI Trends
title_short Warming, Sheep and Volcanoes: Land Cover Changes in Iceland Evident in Satellite NDVI Trends
title_sort warming sheep and volcanoes land cover changes in iceland evident in satellite ndvi trends
topic AHVRR
MODIS
land cover
land use
NDVI
url http://www.mdpi.com/2072-4292/7/8/9492
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