Tundra Browning in the Indigirka Lowlands (North-Eastern Siberia) Explained by Drought, Floods and Small-Scale Vegetation Shifts
Contrary to the general “greening of the Arctic”, the Siberian Indigirka Lowlands show strong “browning” (a decrease in the Normalized Difference Vegetation Index or “NDVI”) in various recent satellite records. Since greening and browning are generally indicative of increases and losses in photosynt...
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ftunivwagenin:oai:library.wur.nl:wurpubs/617658 2024-04-28T08:05:34+00:00 Tundra Browning in the Indigirka Lowlands (North-Eastern Siberia) Explained by Drought, Floods and Small-Scale Vegetation Shifts Magnússon, Rúna Groten, Finn Bartholomeus, Harm van Huissteden, Ko Heijmans, Monique M.P.D. 2023 application/pdf https://research.wur.nl/en/publications/tundra-browning-in-the-indigirka-lowlands-north-eastern-siberia-e https://doi.org/10.1029/2022JG007330 en eng https://edepot.wur.nl/636457 https://research.wur.nl/en/publications/tundra-browning-in-the-indigirka-lowlands-north-eastern-siberia-e doi:10.1029/2022JG007330 https://creativecommons.org/licenses/by/4.0/ Wageningen University & Research Journal of Geophysical Research: Biogeosciences 128 (2023) 7 ISSN: 2169-8953 Arctic tundra Landsat NDVI Siberia greening precipitation Article/Letter to editor 2023 ftunivwagenin https://doi.org/10.1029/2022JG007330 2024-04-03T14:26:15Z Contrary to the general “greening of the Arctic”, the Siberian Indigirka Lowlands show strong “browning” (a decrease in the Normalized Difference Vegetation Index or “NDVI”) in various recent satellite records. Since greening and browning are generally indicative of increases and losses in photosynthetically active biomass, this browning trend may have implications for the carbon balance and vegetation of this Arctic tundra region. To explore potential mechanisms responsible for this trend break from general Arctic greening, we studied timeseries of Landsat summer maximum NDVI, weather data, and high-resolution maps of vegetation compositional change, topography, geomorphology and hydrology. We find that a significant proportion of browning (lower summer NDVI) is explained by moisture dynamics, with high snow depths and resulting floods as well as summer drought coinciding with low NDVI. Relations between seasonal weather variables and NDVI are spatially heterogeneous, with floodplains, drained thaw lake basins and Yedoma ridges showing different patterns of association with weather variables. Low summer NDVI after high snowfall was particularly evident in floodplains, likely explained by early summer floods. Local small-scale vegetation changes explained only small amounts of variance in browning rates in Landsat NDVI. Local expansion of Sphagnum vegetation in particular may have contributed to recent browning of our study site, but higher resolution NDVI timeseries are necessary to accurately constrain the role of small-scale vegetation shifts. Overall, associations identified in this study suggest that future increases in Arctic precipitation variability and extremes may limit tundra greening, but to different extents even across comparatively small topographical contrasts. Article in Journal/Newspaper Arctic Greening Arctic Tundra Siberia Wageningen UR (University & Research Centre): Digital Library Journal of Geophysical Research: Biogeosciences 128 7 |
institution |
Open Polar |
collection |
Wageningen UR (University & Research Centre): Digital Library |
op_collection_id |
ftunivwagenin |
language |
English |
topic |
Arctic tundra Landsat NDVI Siberia greening precipitation |
spellingShingle |
Arctic tundra Landsat NDVI Siberia greening precipitation Magnússon, Rúna Groten, Finn Bartholomeus, Harm van Huissteden, Ko Heijmans, Monique M.P.D. Tundra Browning in the Indigirka Lowlands (North-Eastern Siberia) Explained by Drought, Floods and Small-Scale Vegetation Shifts |
topic_facet |
Arctic tundra Landsat NDVI Siberia greening precipitation |
description |
Contrary to the general “greening of the Arctic”, the Siberian Indigirka Lowlands show strong “browning” (a decrease in the Normalized Difference Vegetation Index or “NDVI”) in various recent satellite records. Since greening and browning are generally indicative of increases and losses in photosynthetically active biomass, this browning trend may have implications for the carbon balance and vegetation of this Arctic tundra region. To explore potential mechanisms responsible for this trend break from general Arctic greening, we studied timeseries of Landsat summer maximum NDVI, weather data, and high-resolution maps of vegetation compositional change, topography, geomorphology and hydrology. We find that a significant proportion of browning (lower summer NDVI) is explained by moisture dynamics, with high snow depths and resulting floods as well as summer drought coinciding with low NDVI. Relations between seasonal weather variables and NDVI are spatially heterogeneous, with floodplains, drained thaw lake basins and Yedoma ridges showing different patterns of association with weather variables. Low summer NDVI after high snowfall was particularly evident in floodplains, likely explained by early summer floods. Local small-scale vegetation changes explained only small amounts of variance in browning rates in Landsat NDVI. Local expansion of Sphagnum vegetation in particular may have contributed to recent browning of our study site, but higher resolution NDVI timeseries are necessary to accurately constrain the role of small-scale vegetation shifts. Overall, associations identified in this study suggest that future increases in Arctic precipitation variability and extremes may limit tundra greening, but to different extents even across comparatively small topographical contrasts. |
format |
Article in Journal/Newspaper |
author |
Magnússon, Rúna Groten, Finn Bartholomeus, Harm van Huissteden, Ko Heijmans, Monique M.P.D. |
author_facet |
Magnússon, Rúna Groten, Finn Bartholomeus, Harm van Huissteden, Ko Heijmans, Monique M.P.D. |
author_sort |
Magnússon, Rúna |
title |
Tundra Browning in the Indigirka Lowlands (North-Eastern Siberia) Explained by Drought, Floods and Small-Scale Vegetation Shifts |
title_short |
Tundra Browning in the Indigirka Lowlands (North-Eastern Siberia) Explained by Drought, Floods and Small-Scale Vegetation Shifts |
title_full |
Tundra Browning in the Indigirka Lowlands (North-Eastern Siberia) Explained by Drought, Floods and Small-Scale Vegetation Shifts |
title_fullStr |
Tundra Browning in the Indigirka Lowlands (North-Eastern Siberia) Explained by Drought, Floods and Small-Scale Vegetation Shifts |
title_full_unstemmed |
Tundra Browning in the Indigirka Lowlands (North-Eastern Siberia) Explained by Drought, Floods and Small-Scale Vegetation Shifts |
title_sort |
tundra browning in the indigirka lowlands (north-eastern siberia) explained by drought, floods and small-scale vegetation shifts |
publishDate |
2023 |
url |
https://research.wur.nl/en/publications/tundra-browning-in-the-indigirka-lowlands-north-eastern-siberia-e https://doi.org/10.1029/2022JG007330 |
genre |
Arctic Greening Arctic Tundra Siberia |
genre_facet |
Arctic Greening Arctic Tundra Siberia |
op_source |
Journal of Geophysical Research: Biogeosciences 128 (2023) 7 ISSN: 2169-8953 |
op_relation |
https://edepot.wur.nl/636457 https://research.wur.nl/en/publications/tundra-browning-in-the-indigirka-lowlands-north-eastern-siberia-e doi:10.1029/2022JG007330 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ Wageningen University & Research |
op_doi |
https://doi.org/10.1029/2022JG007330 |
container_title |
Journal of Geophysical Research: Biogeosciences |
container_volume |
128 |
container_issue |
7 |
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1797575526235242496 |