Wagner J A. The influence of average snow depth on monthlymean temperature anomaly[J].Mon.Wea.Rev,1973,101:624-626.
[14]
Ge Y ,Gong G.. Observed inconsistencies between snow extentand snow depth variability at regional/continental scales[J].J.Climate,2008,21:1066-1082.
[15]
Ge Y,Gong G. .Physical mechanisms linking the winter Pacific-North American teleconnection pattern to spring NorthAmerican snow depth[J].J.Climate,2009.22:5135-5148.
[16]
Kripalani R H, Kulkarni A. Climatology and variability of historicalSoviet snow depth data:Some new perspectives insnow-Indian monsoon teleconnections[J]. Climate Dynamics,1999,15:475-489.
[17]
Ye H, Bao Z. Lagged teleconnections between snow depth innorthern Eurasia,rainfall in Southeast Asia and sea surface temperaturesover the tropical Pacific Ocean[J].International Journalof Climatology,2001,21(13):1607-1621.
Gutzler D S, Rosen R D. Interannual variability of wintertimesnow cover across the Northern Hemisphere[J].J.Climate,1992,5:1441-1447.
[20]
Serreze M C, McGinnis D, Robinson D. Characteristics ofsnowfall over the eastern half of the United States and relationshipswith principal modes of low frequency atmospheric variability [J].J. Climate,1998,11:234-250.
[21]
Douville H, Royer J F. Sensitivity of the Asian summer monsoonto an anomalous Eurasian snow cover within the Météo-FranceGCM [J].Climate Dynamics,1996,12 (7):449-466.
Dey B,Bhanu Kumar O S R U.An apparent relationship betweenEurasian spring snow cover and the advance period of the Indiansummer monsoon[J].J.Appl.Meteor,1982,21(12):1929-1932.
