Temperature effects of passive greenhouse apparatus in high-latitude climate change experiments

1. Passive greenhouse apparatus is commonly used to investigate the in situ biological response of terrestrial communities to global warming. 2. Although close conformity of greenhouse treatment effects to general circulation model (GCM) scenarios is widely claimed, no proof of such a relationship h...

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Published in:Functional Ecology
Main Author: Kennedy, A. D.
Format: Article in Journal/Newspaper
Language:unknown
Published: 1995
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/515727/
https://doi.org/10.2307/2390583
id ftnerc:oai:nora.nerc.ac.uk:515727
record_format openpolar
spelling ftnerc:oai:nora.nerc.ac.uk:515727 2023-05-15T13:49:33+02:00 Temperature effects of passive greenhouse apparatus in high-latitude climate change experiments Kennedy, A. D. 1995-04 http://nora.nerc.ac.uk/id/eprint/515727/ https://doi.org/10.2307/2390583 unknown Kennedy, A. D. 1995 Temperature effects of passive greenhouse apparatus in high-latitude climate change experiments. Functional Ecology, 9 (2). 340-350. https://doi.org/10.2307/2390583 <https://doi.org/10.2307/2390583> Publication - Article PeerReviewed 1995 ftnerc https://doi.org/10.2307/2390583 2023-02-04T19:44:13Z 1. Passive greenhouse apparatus is commonly used to investigate the in situ biological response of terrestrial communities to global warming. 2. Although close conformity of greenhouse treatment effects to general circulation model (GCM) scenarios is widely claimed, no proof of such a relationship has yet been published. 3. Here, the relationship between passive greenhouse thermal environment and future climate conditions is considered using temperature data collected from within and without greenhouses deployed in the maritime Antarctic. It is revealed that in terms of thermal extremes, diel and annual variation, and overall distribution across the temperature spectrum, such apparatus achieves only poor simulation of GCM forecasts. 4. During summer, greenhouses induce an amplified daily range of temperatures, elevated maxima and accelerated rates of change. 5. During spring and autumn, diel temperature variation continues inside the greenhouses while snow cover protects the controls. 6. During winter, an inverse treatment effect occurs, in which the relative depth of snow cover causes lower temperatures in greenhouses than in controls. 7. These treatment effects differ significantly from GCM climate predictions. Changes recorded in the composition, structure and function of greenhouse biota may thus be artefacts of the methodology. 8. Thorough a priori testing of greenhouse treatment effects is recommended for future climate change studies that are to be conducted in environments subject to seasonal snowfall, solar elevation and day length. Article in Journal/Newspaper Antarc* Antarctic Natural Environment Research Council: NERC Open Research Archive Antarctic Functional Ecology 9 2 340
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
description 1. Passive greenhouse apparatus is commonly used to investigate the in situ biological response of terrestrial communities to global warming. 2. Although close conformity of greenhouse treatment effects to general circulation model (GCM) scenarios is widely claimed, no proof of such a relationship has yet been published. 3. Here, the relationship between passive greenhouse thermal environment and future climate conditions is considered using temperature data collected from within and without greenhouses deployed in the maritime Antarctic. It is revealed that in terms of thermal extremes, diel and annual variation, and overall distribution across the temperature spectrum, such apparatus achieves only poor simulation of GCM forecasts. 4. During summer, greenhouses induce an amplified daily range of temperatures, elevated maxima and accelerated rates of change. 5. During spring and autumn, diel temperature variation continues inside the greenhouses while snow cover protects the controls. 6. During winter, an inverse treatment effect occurs, in which the relative depth of snow cover causes lower temperatures in greenhouses than in controls. 7. These treatment effects differ significantly from GCM climate predictions. Changes recorded in the composition, structure and function of greenhouse biota may thus be artefacts of the methodology. 8. Thorough a priori testing of greenhouse treatment effects is recommended for future climate change studies that are to be conducted in environments subject to seasonal snowfall, solar elevation and day length.
format Article in Journal/Newspaper
author Kennedy, A. D.
spellingShingle Kennedy, A. D.
Temperature effects of passive greenhouse apparatus in high-latitude climate change experiments
author_facet Kennedy, A. D.
author_sort Kennedy, A. D.
title Temperature effects of passive greenhouse apparatus in high-latitude climate change experiments
title_short Temperature effects of passive greenhouse apparatus in high-latitude climate change experiments
title_full Temperature effects of passive greenhouse apparatus in high-latitude climate change experiments
title_fullStr Temperature effects of passive greenhouse apparatus in high-latitude climate change experiments
title_full_unstemmed Temperature effects of passive greenhouse apparatus in high-latitude climate change experiments
title_sort temperature effects of passive greenhouse apparatus in high-latitude climate change experiments
publishDate 1995
url http://nora.nerc.ac.uk/id/eprint/515727/
https://doi.org/10.2307/2390583
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation Kennedy, A. D. 1995 Temperature effects of passive greenhouse apparatus in high-latitude climate change experiments. Functional Ecology, 9 (2). 340-350. https://doi.org/10.2307/2390583 <https://doi.org/10.2307/2390583>
op_doi https://doi.org/10.2307/2390583
container_title Functional Ecology
container_volume 9
container_issue 2
container_start_page 340
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