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[1] A highly resolved Mt. Everest ice core reveals a decrease in marine and increase in continental air masses related to relatively high summer surface pressure over Mongolia, and reduction in northward incursions of the summer South Asian monsoon since 1400 AD. Previously published proxy records f...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.455.6081 2023-05-15T16:38:57+02:00 Authors Mt. Everest Ice Core Susan D. Kaspari Paul Andrew Mayewski Shichang Kang Sharon B. Sneed Shugui Hou Roger Hooke J. Kreutz D. Introne Kirk A. Maasch Dahe Qin J. Ren The Pennsylvania State University CiteSeerX Archives http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.455.6081 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.455.6081 Metadata may be used without restrictions as long as the oai identifier remains attached to it. text ftciteseerx 2016-01-08T06:10:20Z [1] A highly resolved Mt. Everest ice core reveals a decrease in marine and increase in continental air masses related to relatively high summer surface pressure over Mongolia, and reduction in northward incursions of the summer South Asian monsoon since 1400 AD. Previously published proxy records from lower sites south of the Himalayas indicate strengthening of the monsoon since this time. These regional differences are consistent with a south– north seesaw in convective activity in the Asian monsoon region, and reflect a southward shift in the mean summer position of themonsoon trough since1400AD. The change in monsoonal circulation at 1400 AD is synchronous with a Text ice core Unknown |
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[1] A highly resolved Mt. Everest ice core reveals a decrease in marine and increase in continental air masses related to relatively high summer surface pressure over Mongolia, and reduction in northward incursions of the summer South Asian monsoon since 1400 AD. Previously published proxy records from lower sites south of the Himalayas indicate strengthening of the monsoon since this time. These regional differences are consistent with a south– north seesaw in convective activity in the Asian monsoon region, and reflect a southward shift in the mean summer position of themonsoon trough since1400AD. The change in monsoonal circulation at 1400 AD is synchronous with a |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
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Mt. Everest Ice Core Susan D. Kaspari Paul Andrew Mayewski Shichang Kang Sharon B. Sneed Shugui Hou Roger Hooke J. Kreutz D. Introne Kirk A. Maasch Dahe Qin J. Ren |
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Mt. Everest Ice Core Susan D. Kaspari Paul Andrew Mayewski Shichang Kang Sharon B. Sneed Shugui Hou Roger Hooke J. Kreutz D. Introne Kirk A. Maasch Dahe Qin J. Ren Authors |
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Mt. Everest Ice Core Susan D. Kaspari Paul Andrew Mayewski Shichang Kang Sharon B. Sneed Shugui Hou Roger Hooke J. Kreutz D. Introne Kirk A. Maasch Dahe Qin J. Ren |
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Mt. Everest |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.455.6081 |
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ice core |
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ice core |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.455.6081 |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766029307212201984 |