Iceland as a heat island
[1] Iceland is a strong localized source of non-eruptive volcanic warming and cooling. Temperature trend maps show that this phenomenon is localized to an area of about twice that of Iceland. With altitude the area remains constant but the phenomenon weakens and changes sign upon passing through the...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.394.9977 http://www.pas.rochester.edu/~douglass/papers/2004GL021816_Iceland.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.394.9977 2023-05-15T16:43:08+02:00 Iceland as a heat island D. H. Douglass V. Patel R. S. Knox The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.394.9977 http://www.pas.rochester.edu/~douglass/papers/2004GL021816_Iceland.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.394.9977 http://www.pas.rochester.edu/~douglass/papers/2004GL021816_Iceland.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.pas.rochester.edu/~douglass/papers/2004GL021816_Iceland.pdf text ftciteseerx 2016-01-08T02:26:01Z [1] Iceland is a strong localized source of non-eruptive volcanic warming and cooling. Temperature trend maps show that this phenomenon is localized to an area of about twice that of Iceland. With altitude the area remains constant but the phenomenon weakens and changes sign upon passing through the tropopause. The effect’s magnitude implies a large positive feedback, according to a conventional climate forcing estimate. This phenomenon is unique in that it is not observed for the other major Text Iceland Unknown |
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ftciteseerx |
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English |
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[1] Iceland is a strong localized source of non-eruptive volcanic warming and cooling. Temperature trend maps show that this phenomenon is localized to an area of about twice that of Iceland. With altitude the area remains constant but the phenomenon weakens and changes sign upon passing through the tropopause. The effect’s magnitude implies a large positive feedback, according to a conventional climate forcing estimate. This phenomenon is unique in that it is not observed for the other major |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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D. H. Douglass V. Patel R. S. Knox |
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D. H. Douglass V. Patel R. S. Knox Iceland as a heat island |
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D. H. Douglass V. Patel R. S. Knox |
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D. H. Douglass |
| title |
Iceland as a heat island |
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Iceland as a heat island |
| title_full |
Iceland as a heat island |
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Iceland as a heat island |
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Iceland as a heat island |
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iceland as a heat island |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.394.9977 http://www.pas.rochester.edu/~douglass/papers/2004GL021816_Iceland.pdf |
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Iceland |
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Iceland |
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http://www.pas.rochester.edu/~douglass/papers/2004GL021816_Iceland.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.394.9977 http://www.pas.rochester.edu/~douglass/papers/2004GL021816_Iceland.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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