41SOLA, 2010, Vol. 6, 041−044, doi:10.2151/sola.2010-011 The summer Arctic sea ice extent (SIE) during the period 1996−2008 had an accelerating trend of retreat. The difference of SIE between May and September has a significant correlation with the summer Northern Hemisphere Annular Mode (summer NAM...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.462.6036 2023-05-15T14:40:48+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.462.6036 http://eprints2008.lib.hokudai.ac.jp/dspace/bitstream/2115/43136/1/SOLA6_41-44.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.462.6036 http://eprints2008.lib.hokudai.ac.jp/dspace/bitstream/2115/43136/1/SOLA6_41-44.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://eprints2008.lib.hokudai.ac.jp/dspace/bitstream/2115/43136/1/SOLA6_41-44.pdf text ftciteseerx 2016-10-16T00:04:52Z 41SOLA, 2010, Vol. 6, 041−044, doi:10.2151/sola.2010-011 The summer Arctic sea ice extent (SIE) during the period 1996−2008 had an accelerating trend of retreat. The difference of SIE between May and September has a significant correlation with the summer Northern Hemisphere Annular Mode (summer NAM). The summer NAM had a significant positive trend during the period 1958−1996, and a weak negative trend during the period 1996−2008. The atmospheric circulation during the recent period had a trend of anticyclonic circulation over the Arctic with easterly wind over the marginal seas. In addition, tropospheric warming was enhanced especially over the Arctic and near the ground surface. 1. Text Arctic Sea ice Unknown Arctic Sola ENVELOPE(9.806,9.806,63.198,63.198) |
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ftciteseerx |
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English |
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41SOLA, 2010, Vol. 6, 041−044, doi:10.2151/sola.2010-011 The summer Arctic sea ice extent (SIE) during the period 1996−2008 had an accelerating trend of retreat. The difference of SIE between May and September has a significant correlation with the summer Northern Hemisphere Annular Mode (summer NAM). The summer NAM had a significant positive trend during the period 1958−1996, and a weak negative trend during the period 1996−2008. The atmospheric circulation during the recent period had a trend of anticyclonic circulation over the Arctic with easterly wind over the marginal seas. In addition, tropospheric warming was enhanced especially over the Arctic and near the ground surface. 1. |
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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=10.1.1.462.6036 http://eprints2008.lib.hokudai.ac.jp/dspace/bitstream/2115/43136/1/SOLA6_41-44.pdf |
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ENVELOPE(9.806,9.806,63.198,63.198) |
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Arctic Sola |
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Arctic Sola |
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Arctic Sea ice |
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Arctic Sea ice |
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http://eprints2008.lib.hokudai.ac.jp/dspace/bitstream/2115/43136/1/SOLA6_41-44.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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