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Microclimatic Performance of a Free-Air Warming and CO(2) Enrichment Experiment in Windy Wyoming, USA
In order to plan for global changing climate experiments are being conducted in many countries, but few have monitored the effects of the climate change treatments (warming, elevated CO(2)) on the experimental plot microclimate. During three years of an eight year study with year-round feedback-cont...
Autores principales: | , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Public Library of Science
2015
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4319967/ https://www.ncbi.nlm.nih.gov/pubmed/25658313 http://dx.doi.org/10.1371/journal.pone.0116834 |
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author | LeCain, Daniel Smith, David Morgan, Jack Kimball, Bruce A. Pendall, Elise Miglietta, Franco |
author_facet | LeCain, Daniel Smith, David Morgan, Jack Kimball, Bruce A. Pendall, Elise Miglietta, Franco |
author_sort | LeCain, Daniel |
collection | PubMed |
description | In order to plan for global changing climate experiments are being conducted in many countries, but few have monitored the effects of the climate change treatments (warming, elevated CO(2)) on the experimental plot microclimate. During three years of an eight year study with year-round feedback-controlled infra-red heater warming (1.5/3.0°C day/night) and growing season free-air CO(2) enrichment (600 ppm) in the mixed-grass prairie of Wyoming, USA, we monitored soil, leaf, canopy-air, above-canopy-air temperatures and relative humidity of control and treated experimental plots and evaluated ecologically important temperature differentials. Leaves were warmed somewhat less than the target settings (1.1 & 1.5°C day/night) but soil was warmed more creating an average that matched the target settings extremely well both during the day and night plus the summer and winter. The site typically has about 50% bare or litter covered soil, therefore soil heat transfer is more critical than in dense canopy ecosystems. The Wyoming site commonly has strong winds (5 ms(-1) average) and significant daily and seasonal temperature fluctuations (as much as 30°C daily) but the warming system was nearly always able to maintain the set temperatures regardless of abiotic variation. The within canopy-air was only slightly warmed and above canopy-air was not warmed by the system, therefore convective warming was minor. Elevated CO(2) had no direct effect nor interaction with the warming treatment on microclimate. Relative humidity within the plant canopy was only slightly reduced by warming. Soil water content was reduced by warming but increased by elevated CO(2). This study demonstrates the importance of monitoring the microclimate in manipulative field global change experiments so that critical physiological and ecological conclusions can be determined. Highly variable energy demand fluctuations showed that passive IR heater warming systems will not maintain desired warming for much of the time. |
format | Online Article Text |
id | pubmed-4319967 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2015 |
publisher | Public Library of Science |
record_format | MEDLINE/PubMed |
spelling | pubmed-43199672015-02-18 Microclimatic Performance of a Free-Air Warming and CO(2) Enrichment Experiment in Windy Wyoming, USA LeCain, Daniel Smith, David Morgan, Jack Kimball, Bruce A. Pendall, Elise Miglietta, Franco PLoS One Research Article In order to plan for global changing climate experiments are being conducted in many countries, but few have monitored the effects of the climate change treatments (warming, elevated CO(2)) on the experimental plot microclimate. During three years of an eight year study with year-round feedback-controlled infra-red heater warming (1.5/3.0°C day/night) and growing season free-air CO(2) enrichment (600 ppm) in the mixed-grass prairie of Wyoming, USA, we monitored soil, leaf, canopy-air, above-canopy-air temperatures and relative humidity of control and treated experimental plots and evaluated ecologically important temperature differentials. Leaves were warmed somewhat less than the target settings (1.1 & 1.5°C day/night) but soil was warmed more creating an average that matched the target settings extremely well both during the day and night plus the summer and winter. The site typically has about 50% bare or litter covered soil, therefore soil heat transfer is more critical than in dense canopy ecosystems. The Wyoming site commonly has strong winds (5 ms(-1) average) and significant daily and seasonal temperature fluctuations (as much as 30°C daily) but the warming system was nearly always able to maintain the set temperatures regardless of abiotic variation. The within canopy-air was only slightly warmed and above canopy-air was not warmed by the system, therefore convective warming was minor. Elevated CO(2) had no direct effect nor interaction with the warming treatment on microclimate. Relative humidity within the plant canopy was only slightly reduced by warming. Soil water content was reduced by warming but increased by elevated CO(2). This study demonstrates the importance of monitoring the microclimate in manipulative field global change experiments so that critical physiological and ecological conclusions can be determined. Highly variable energy demand fluctuations showed that passive IR heater warming systems will not maintain desired warming for much of the time. Public Library of Science 2015-02-06 /pmc/articles/PMC4319967/ /pubmed/25658313 http://dx.doi.org/10.1371/journal.pone.0116834 Text en https://creativecommons.org/publicdomain/zero/1.0/ This is an open-access article distributed under the terms of the Creative Commons Public Domain declaration, which stipulates that, once placed in the public domain, this work may be freely reproduced, distributed, transmitted, modified, built upon, or otherwise used by anyone for any lawful purpose. |
spellingShingle | Research Article LeCain, Daniel Smith, David Morgan, Jack Kimball, Bruce A. Pendall, Elise Miglietta, Franco Microclimatic Performance of a Free-Air Warming and CO(2) Enrichment Experiment in Windy Wyoming, USA |
title | Microclimatic Performance of a Free-Air Warming and CO(2) Enrichment Experiment in Windy Wyoming, USA |
title_full | Microclimatic Performance of a Free-Air Warming and CO(2) Enrichment Experiment in Windy Wyoming, USA |
title_fullStr | Microclimatic Performance of a Free-Air Warming and CO(2) Enrichment Experiment in Windy Wyoming, USA |
title_full_unstemmed | Microclimatic Performance of a Free-Air Warming and CO(2) Enrichment Experiment in Windy Wyoming, USA |
title_short | Microclimatic Performance of a Free-Air Warming and CO(2) Enrichment Experiment in Windy Wyoming, USA |
title_sort | microclimatic performance of a free-air warming and co(2) enrichment experiment in windy wyoming, usa |
topic | Research Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4319967/ https://www.ncbi.nlm.nih.gov/pubmed/25658313 http://dx.doi.org/10.1371/journal.pone.0116834 |
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