Tibetan alpine tundra responses to simulated changes in climate: Aboveground biomass and community responses

High-elevation ecosystems are predicted to be some of the terrestrial habitats most sensitive to changing climates. The ecological consequences of changes in alpine tundra environmental conditions are still unclear especially for habitats in Asia. In this study we report findings from a field experi...

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Main Authors: Zhang, YQ, Welker, JM
Format: Report
Language:unknown
Published: INST ARCTIC ALPINE RES 1996
Subjects:
Online Access:http://210.75.249.4/handle/363003/13269
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spelling ftchinacascnwipb:oai:210.75.249.4:363003/18656 2023-05-15T14:20:20+02:00 Tibetan alpine tundra responses to simulated changes in climate: Aboveground biomass and community responses Zhang, YQ Welker, JM 1996-05-01 http://210.75.249.4/handle/363003/13269 unknown INST ARCTIC ALPINE RES ARCTIC AND ALPINE RESEARCH http://210.75.249.4/handle/363003/13269 期刊论文 1996 ftchinacascnwipb 2023-03-26T20:26:26Z High-elevation ecosystems are predicted to be some of the terrestrial habitats most sensitive to changing climates. The ecological consequences of changes in alpine tundra environmental conditions are still unclear especially for habitats in Asia. In this study we report findings from a field experiment where an alpine tundra grassland on the Tibetan plateau (37 degrees N, 101 degrees E) was exposed to experimental warming, irradiance was lowered, and wind speed reduced to simulate a suite of potential changes in environmental conditions. Our warming treatment increased air temperatures by 5 degrees C on average and soil temperatures were elevated by 3 degrees C at 5 cm depth. Aboveground biomass of grasses responded rapidly to the warmer conditions whereby biomass was 25% greater than that of controls after only 5 wk of experimental warming. This increase was accompanied by a simultaneous decrease in forb biomass, resulting in almost no net change in community biomass after 5 wk. Lower irradiance reduced grass biomass during the same period. Under ambient conditions total aboveground community biomass increased seasonally from 161 g m(-2) in July to a maximum of 351 g m(-2) in September, declining to 285 g m(-2) in October. However, under warmed conditions, peak community biomass was extended into October due in part to continued growth of grasses and the postponement of senescence. Our findings indicate that while alpine grasses respond favorably to altered conditions, others may not. And, while peak community biomass may actually change very little under warmer summers, the duration of peak biomass may be extended having feedback effects on net ecosystem CO2 balances, nutrient cycling, and forage availability. Report Arctic Arctic and Alpine Research Tundra Northwest Institute of Plateau Biology: NWIPB OpenIR (Chinese Academy of Sciences)
institution Open Polar
collection Northwest Institute of Plateau Biology: NWIPB OpenIR (Chinese Academy of Sciences)
op_collection_id ftchinacascnwipb
language unknown
description High-elevation ecosystems are predicted to be some of the terrestrial habitats most sensitive to changing climates. The ecological consequences of changes in alpine tundra environmental conditions are still unclear especially for habitats in Asia. In this study we report findings from a field experiment where an alpine tundra grassland on the Tibetan plateau (37 degrees N, 101 degrees E) was exposed to experimental warming, irradiance was lowered, and wind speed reduced to simulate a suite of potential changes in environmental conditions. Our warming treatment increased air temperatures by 5 degrees C on average and soil temperatures were elevated by 3 degrees C at 5 cm depth. Aboveground biomass of grasses responded rapidly to the warmer conditions whereby biomass was 25% greater than that of controls after only 5 wk of experimental warming. This increase was accompanied by a simultaneous decrease in forb biomass, resulting in almost no net change in community biomass after 5 wk. Lower irradiance reduced grass biomass during the same period. Under ambient conditions total aboveground community biomass increased seasonally from 161 g m(-2) in July to a maximum of 351 g m(-2) in September, declining to 285 g m(-2) in October. However, under warmed conditions, peak community biomass was extended into October due in part to continued growth of grasses and the postponement of senescence. Our findings indicate that while alpine grasses respond favorably to altered conditions, others may not. And, while peak community biomass may actually change very little under warmer summers, the duration of peak biomass may be extended having feedback effects on net ecosystem CO2 balances, nutrient cycling, and forage availability.
format Report
author Zhang, YQ
Welker, JM
spellingShingle Zhang, YQ
Welker, JM
Tibetan alpine tundra responses to simulated changes in climate: Aboveground biomass and community responses
author_facet Zhang, YQ
Welker, JM
author_sort Zhang, YQ
title Tibetan alpine tundra responses to simulated changes in climate: Aboveground biomass and community responses
title_short Tibetan alpine tundra responses to simulated changes in climate: Aboveground biomass and community responses
title_full Tibetan alpine tundra responses to simulated changes in climate: Aboveground biomass and community responses
title_fullStr Tibetan alpine tundra responses to simulated changes in climate: Aboveground biomass and community responses
title_full_unstemmed Tibetan alpine tundra responses to simulated changes in climate: Aboveground biomass and community responses
title_sort tibetan alpine tundra responses to simulated changes in climate: aboveground biomass and community responses
publisher INST ARCTIC ALPINE RES
publishDate 1996
url http://210.75.249.4/handle/363003/13269
genre Arctic
Arctic and Alpine Research
Tundra
genre_facet Arctic
Arctic and Alpine Research
Tundra
op_relation ARCTIC AND ALPINE RESEARCH
http://210.75.249.4/handle/363003/13269
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