Freeze and breakup dates of ice on Lakes and rivers provide consistent evid
ence of Later freezing and earlier breakup around the Northern Hemisphere f
rom 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 ab
out 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 re
duced ice cover (a warming trend) beginning as early as the 16th century, w
ith increasing rates of change after about 1850.