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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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 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
http://www.ouce.ox.ac.uk/~rwashing/research/publications/tenerife.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.560.3502 http://www.ouce.ox.ac.uk/~rwashing/research/publications/tenerife.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766132668020293632 |