REFERENCES
associated with the circulation patterns shown in figure 11. During winter the very strong ridge and northerly direction of the height arionialy (fig. 11A) favored repeated, strong outbreaks of Arctic air masses. In spring (fig. 11B) heights were below nornial in western Canada and there was a troug...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.395.2677 2023-05-15T14:59:01+02:00 REFERENCES J. Xarnias Persisteiice Of Mid-tropospheric Circulations Between The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.2677 http://docs.lib.noaa.gov/rescue/mwr/091/mwr-091-08-0410.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.2677 http://docs.lib.noaa.gov/rescue/mwr/091/mwr-091-08-0410.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://docs.lib.noaa.gov/rescue/mwr/091/mwr-091-08-0410.pdf the Sea in Motion The Rossby Memorial Volume Rockefeller text ftciteseerx 2016-01-08T02:26:34Z associated with the circulation patterns shown in figure 11. During winter the very strong ridge and northerly direction of the height arionialy (fig. 11A) favored repeated, strong outbreaks of Arctic air masses. In spring (fig. 11B) heights were below nornial in western Canada and there was a trough along the west coast. These conditions encourage warmth east of the Rockies. Compared with the winter season, spring was rather unspectacular with few new records. Reno, A’ev., reported the wettest spring since records began with inore than three times norinal rainfall associated with the coastal trough. Other records include the warmest spring at Text Arctic Unknown Arctic Canada Reno ENVELOPE(-117.003,-117.003,56.000,56.000) |
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Unknown |
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ftciteseerx |
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English |
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the Sea in Motion The Rossby Memorial Volume Rockefeller |
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the Sea in Motion The Rossby Memorial Volume Rockefeller J. Xarnias Persisteiice Of Mid-tropospheric Circulations Between REFERENCES |
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the Sea in Motion The Rossby Memorial Volume Rockefeller |
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associated with the circulation patterns shown in figure 11. During winter the very strong ridge and northerly direction of the height arionialy (fig. 11A) favored repeated, strong outbreaks of Arctic air masses. In spring (fig. 11B) heights were below nornial in western Canada and there was a trough along the west coast. These conditions encourage warmth east of the Rockies. Compared with the winter season, spring was rather unspectacular with few new records. Reno, A’ev., reported the wettest spring since records began with inore than three times norinal rainfall associated with the coastal trough. Other records include the warmest spring at |
author2 |
The Pennsylvania State University CiteSeerX Archives |
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Text |
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J. Xarnias Persisteiice Of Mid-tropospheric Circulations Between |
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J. Xarnias Persisteiice Of Mid-tropospheric Circulations Between |
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J. Xarnias |
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REFERENCES |
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REFERENCES |
title_full |
REFERENCES |
title_fullStr |
REFERENCES |
title_full_unstemmed |
REFERENCES |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.2677 http://docs.lib.noaa.gov/rescue/mwr/091/mwr-091-08-0410.pdf |
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ENVELOPE(-117.003,-117.003,56.000,56.000) |
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Arctic Canada Reno |
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Arctic Canada Reno |
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Arctic |
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Arctic |
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http://docs.lib.noaa.gov/rescue/mwr/091/mwr-091-08-0410.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.2677 http://docs.lib.noaa.gov/rescue/mwr/091/mwr-091-08-0410.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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