are present at all heights, reaching the upper-most levels of the stratosphere (Fig. 4C). There is also evidence of more isolated mountain wave activity over the Alps and the Alaska-Yukon region. Mountain waves are largely absent in both the observations and model results over other mountainous regi...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.637.6986 http://www.atmos.umd.edu/~zeng/papers/znlt99.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.637.6986 2023-05-15T16:28:04+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.637.6986 http://www.atmos.umd.edu/~zeng/papers/znlt99.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.637.6986 http://www.atmos.umd.edu/~zeng/papers/znlt99.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.atmos.umd.edu/~zeng/papers/znlt99.pdf text ftciteseerx 2016-01-08T15:46:39Z are present at all heights, reaching the upper-most levels of the stratosphere (Fig. 4C). There is also evidence of more isolated mountain wave activity over the Alps and the Alaska-Yukon region. Mountain waves are largely absent in both the observations and model results over other mountainous regions, such as western North America, the Hima-layas, Greenland, and Scandinavia. This absence occurs in the MWFM results be-cause regional winds inhibit mountain wave propagation into the stratosphere. Despite the basic similarities, specific dif-ferences between the CRISTA data and MWFM results are also evident in Figs. 3 and Text Greenland Alaska Yukon Unknown Greenland Isolated Mountain ENVELOPE(-126.604,-126.604,56.550,56.550) Yukon |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
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are present at all heights, reaching the upper-most levels of the stratosphere (Fig. 4C). There is also evidence of more isolated mountain wave activity over the Alps and the Alaska-Yukon region. Mountain waves are largely absent in both the observations and model results over other mountainous regions, such as western North America, the Hima-layas, Greenland, and Scandinavia. This absence occurs in the MWFM results be-cause regional winds inhibit mountain wave propagation into the stratosphere. Despite the basic similarities, specific dif-ferences between the CRISTA data and MWFM results are also evident in Figs. 3 and |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.637.6986 http://www.atmos.umd.edu/~zeng/papers/znlt99.pdf |
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ENVELOPE(-126.604,-126.604,56.550,56.550) |
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Greenland Isolated Mountain Yukon |
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Greenland Isolated Mountain Yukon |
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Greenland Alaska Yukon |
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Greenland Alaska Yukon |
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http://www.atmos.umd.edu/~zeng/papers/znlt99.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.637.6986 http://www.atmos.umd.edu/~zeng/papers/znlt99.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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