Magnuson JJ, Robertson DM, Benson BJ, Wynne RH, Livingstone DM, Arai T, Assel RA, Barry RG, Card V, Kuusisto E, Granin NG, Prowse TD, Stewart KM, Vuglinski VS
Center for Limnology, University of Wisconsin-Madison, Madison, WI 53706, USA. U.S. Geological Survey, Water Resources Division, 8505 Research Way, Middleton, WI 53562, USA. Department of Forestry, Virginia Polytechnic Institute and State Unive.
Science. 2000 Sep 8;289(5485):1743-6. doi: 10.1126/science.289.5485.1743.
Freeze and breakup dates of ice on lakes and rivers provide consistent evidence of later freezing and earlier breakup around the Northern Hemisphere from 1846 to 1995. Over these 150 years, changes in freeze dates averaged 5.8 days per 100 years later, and changes in breakup dates averaged 6.5 days per 100 years earlier; these translate to increasing air temperatures of about 1.2 degrees C per 100 years. Interannual variability in both freeze and breakup dates has increased since 1950. A few longer time series reveal reduced ice cover (a warming trend) beginning as early as the 16th century, with increasing rates of change after about 1850.
1846年至1995年期间,湖泊和河流上冰的冻结和解冻日期提供了一致的证据,表明北半球各地结冰时间推迟、解冻时间提前。在这150年里,冻结日期的变化平均每100年推迟5.8天,解冻日期的变化平均每100年提前6.5天;这相当于气温每100年升高约1.2摄氏度。自1950年以来,冻结和解冻日期的年际变率都有所增加。一些更长的时间序列显示,早在16世纪就开始出现冰盖减少(变暖趋势),1850年左右之后变化速率加快。