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Extra resources for Oxford Reading Tree: Stage 3: More Stories: Snowman (Oxford Reading Tree)

Sample text

Xie et al. [1994] have also found stronglinks would expect spring seasonswith more sea ice to be between ENSO indices and sea ice extent anomalies thosewith coldertemperatures in the lower troposphere. Weddell Sea,as have Yuanand Martinson [2000] for the This would mean (via the hydrostaticequation) that Weddell and ABS. In addition,Bromwichet al. [2000] geopotentialheight anomalieswould becomeprogres- haveconfirmedstrongcorrelations betweenthe moisture sively more negative with height. In fact, the Figure budget over the broaderWest Antarctic sectorand the exhibitsthe oppositeof this (correlationsincreasearith- Southern Oscillation Index.

22, 291-310, 2002. 1997. , T. A. Lachlan-Cope,G. J. Marshall,E. M. Morris, R. Mulvaney, and W. Winter, Spatial variability of Antarctic Peninsulanet surface mass balance, J. , 317, 1978. , and M. R. M. van Lipzig, Responseof anomalies,J. , 44, 877-901, 1987. , The influence of the Antarctic Peninsula on the Oscillation:resultsof a regionalclimate model. (this volwind field over the westernWeddellSea,J. , ume) 88, 2684-2692, 1983. , andH. E. J. Zwally,Antarcticseaice variations and seasonalair temperaturerelationships,or.

Held and T. L. Delworth, Southern Harangozo,S. , Atmosphericmeridionalcirculationimpacts Hemisphereatmosphericcirculation responseto global on contrasting winterseaice extentin two yearsin thePacific warming,J. Climate, 14, 2238-2249, 2001. sectorof the SouthernOcean, Tellus,49A, 388-400, 1997. Harangozo,S. , and J. C. Comiso, SouthernOcean climate and sea ice anomalies associatedwith the Southern Oscillation, J. west Antarctic Peninsula climate in Austral winter, Int. J. Climate, 15, 487-501, 2002.

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