The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive) ...
Table 1. The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive). CH 4 values are for the wetland fraction of the study area only. Abstract One major challenge to the improvement of regional climate scenarios for the northern high latitudes...
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ftdatacite:10.6084/m9.figshare.1011565 2024-04-28T08:07:53+00:00 The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive) ... Zhang, Wenxin Paul A Miller Benjamin Smith Rita Wania Torben Koenigk Döscher, Ralf 2013 https://dx.doi.org/10.6084/m9.figshare.1011565 https://iop.figshare.com/articles/dataset/___The_NEE_and_CH_sub_4_sub_flux_simulated_by_the_CRU_forced_run_and_the_RCAO_forced_run_uptake_nega/1011565 unknown IOP Publishing Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Other environmental sciences not elsewhere classified dataset Dataset 2013 ftdatacite https://doi.org/10.6084/m9.figshare.1011565 2024-04-02T12:12:00Z Table 1. The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive). CH 4 values are for the wetland fraction of the study area only. Abstract One major challenge to the improvement of regional climate scenarios for the northern high latitudes is to understand land surface feedbacks associated with vegetation shifts and ecosystem biogeochemical cycling. We employed a customized, Arctic version of the individual-based dynamic vegetation model LPJ-GUESS to simulate the dynamics of upland and wetland ecosystems under a regional climate model–downscaled future climate projection for the Arctic and Subarctic. The simulated vegetation distribution (1961–1990) agreed well with a composite map of actual arctic vegetation. In the future (2051–2080), a poleward advance of the forest–tundra boundary, an expansion of tall shrub tundra, and a dominance shift from deciduous to evergreen boreal conifer forest over northern Eurasia were simulated. Ecosystems continued ... Dataset Arctic Subarctic Tundra DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Other environmental sciences not elsewhere classified |
spellingShingle |
Other environmental sciences not elsewhere classified Zhang, Wenxin Paul A Miller Benjamin Smith Rita Wania Torben Koenigk Döscher, Ralf The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive) ... |
topic_facet |
Other environmental sciences not elsewhere classified |
description |
Table 1. The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive). CH 4 values are for the wetland fraction of the study area only. Abstract One major challenge to the improvement of regional climate scenarios for the northern high latitudes is to understand land surface feedbacks associated with vegetation shifts and ecosystem biogeochemical cycling. We employed a customized, Arctic version of the individual-based dynamic vegetation model LPJ-GUESS to simulate the dynamics of upland and wetland ecosystems under a regional climate model–downscaled future climate projection for the Arctic and Subarctic. The simulated vegetation distribution (1961–1990) agreed well with a composite map of actual arctic vegetation. In the future (2051–2080), a poleward advance of the forest–tundra boundary, an expansion of tall shrub tundra, and a dominance shift from deciduous to evergreen boreal conifer forest over northern Eurasia were simulated. Ecosystems continued ... |
format |
Dataset |
author |
Zhang, Wenxin Paul A Miller Benjamin Smith Rita Wania Torben Koenigk Döscher, Ralf |
author_facet |
Zhang, Wenxin Paul A Miller Benjamin Smith Rita Wania Torben Koenigk Döscher, Ralf |
author_sort |
Zhang, Wenxin |
title |
The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive) ... |
title_short |
The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive) ... |
title_full |
The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive) ... |
title_fullStr |
The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive) ... |
title_full_unstemmed |
The NEE and CH 4 flux simulated by the CRU-forced run and the RCAO-forced run (uptake: negative, release: positive) ... |
title_sort |
nee and ch 4 flux simulated by the cru-forced run and the rcao-forced run (uptake: negative, release: positive) ... |
publisher |
IOP Publishing |
publishDate |
2013 |
url |
https://dx.doi.org/10.6084/m9.figshare.1011565 https://iop.figshare.com/articles/dataset/___The_NEE_and_CH_sub_4_sub_flux_simulated_by_the_CRU_forced_run_and_the_RCAO_forced_run_uptake_nega/1011565 |
genre |
Arctic Subarctic Tundra |
genre_facet |
Arctic Subarctic Tundra |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.6084/m9.figshare.1011565 |
_version_ |
1797576841807003648 |