Future climate change of the subtropical North Atlantic: implications for the cloud forests of tenerife

Abstract. This paper is concerned with climate change in the region of the Canary Islands and the potential implications for the laurel forests of Tenerife. Frequent orographic cloud formation during the dry season is of vital importance to the altitudinal distribution of the laurel forests, because...

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Main Authors: Frank N. Sperling, Richard Washington, Robert J. Whittaker
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2004
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.560.3502
http://www.ouce.ox.ac.uk/~rwashing/research/publications/tenerife.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.560.3502 2023-05-15T17:33:59+02:00 Future climate change of the subtropical North Atlantic: implications for the cloud forests of tenerife Frank N. Sperling Richard Washington Robert J. Whittaker The Pennsylvania State University CiteSeerX Archives 2004 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.560.3502 http://www.ouce.ox.ac.uk/~rwashing/research/publications/tenerife.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.560.3502 http://www.ouce.ox.ac.uk/~rwashing/research/publications/tenerife.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ouce.ox.ac.uk/~rwashing/research/publications/tenerife.pdf text 2004 ftciteseerx 2016-01-08T12:00:59Z Abstract. This paper is concerned with climate change in the region of the Canary Islands and the potential implications for the laurel forests of Tenerife. Frequent orographic cloud formation during the dry season is of vital importance to the altitudinal distribution of the laurel forests, because it maintains a semi-humid environment in the otherwise semi-arid climate of the Canary Islands. The distinctive environmental conditions in conjunction with the location of the Canary Islands on the Northern poleward edge of the Hadley Circulation make these ecosystems potentially highly sensitive to regional changes in climatic conditions. To explore this sensitivity, we first quantify observed trends in humidity and temperature across an altitudinal transect at the base of the Anaga peninsular, and second, analyse the results of three GCM experiments (CGCM1, ECHAM4 and CSIRO) to develop alternative climate change scenarios, and third, use these data to assess likely shifts in the elevational distribution of the laurel forest climate envelope. We report a significant increase in relative humidity and decreases in the diurnal temperature range on Tenerife at altitudes below the trade wind inversion within the last 30 years during the dry season, which suggests an increased occurrence of low-level clouds. There is also partial evidence for a drying trend across the trade wind inversion, which may be linked to an increased subsidence. Overall, the models suggest a Text North Atlantic Unknown
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description Abstract. This paper is concerned with climate change in the region of the Canary Islands and the potential implications for the laurel forests of Tenerife. Frequent orographic cloud formation during the dry season is of vital importance to the altitudinal distribution of the laurel forests, because it maintains a semi-humid environment in the otherwise semi-arid climate of the Canary Islands. The distinctive environmental conditions in conjunction with the location of the Canary Islands on the Northern poleward edge of the Hadley Circulation make these ecosystems potentially highly sensitive to regional changes in climatic conditions. To explore this sensitivity, we first quantify observed trends in humidity and temperature across an altitudinal transect at the base of the Anaga peninsular, and second, analyse the results of three GCM experiments (CGCM1, ECHAM4 and CSIRO) to develop alternative climate change scenarios, and third, use these data to assess likely shifts in the elevational distribution of the laurel forest climate envelope. We report a significant increase in relative humidity and decreases in the diurnal temperature range on Tenerife at altitudes below the trade wind inversion within the last 30 years during the dry season, which suggests an increased occurrence of low-level clouds. There is also partial evidence for a drying trend across the trade wind inversion, which may be linked to an increased subsidence. Overall, the models suggest a
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Frank N. Sperling
Richard Washington
Robert J. Whittaker
spellingShingle Frank N. Sperling
Richard Washington
Robert J. Whittaker
Future climate change of the subtropical North Atlantic: implications for the cloud forests of tenerife
author_facet Frank N. Sperling
Richard Washington
Robert J. Whittaker
author_sort Frank N. Sperling
title Future climate change of the subtropical North Atlantic: implications for the cloud forests of tenerife
title_short Future climate change of the subtropical North Atlantic: implications for the cloud forests of tenerife
title_full Future climate change of the subtropical North Atlantic: implications for the cloud forests of tenerife
title_fullStr Future climate change of the subtropical North Atlantic: implications for the cloud forests of tenerife
title_full_unstemmed Future climate change of the subtropical North Atlantic: implications for the cloud forests of tenerife
title_sort future climate change of the subtropical north atlantic: implications for the cloud forests of tenerife
publishDate 2004
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.560.3502
http://www.ouce.ox.ac.uk/~rwashing/research/publications/tenerife.pdf
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http://www.ouce.ox.ac.uk/~rwashing/research/publications/tenerife.pdf
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