How about the Roman Warm Period era, when Arctic temperatures were 2 to 6 degrees C warmer than now and the Arctic had less than 50 % sea ice coverage 6 months of the year vs. just 1.5 months of < 50 %
sea ice coverage during the post-1950s «Anthropocene»?
If you'll recall from my previous post, polar bears seem to have barely survived the extensive
sea ice coverage during the Last Glacial Maximum — in other words, too much ice (even over the short term) is their biggest threat.
Not exact matches
During the so - called Holocene Climate Optimum, from approximately 8000 to 5000 years ago, when the temperatures were somewhat warmer than today, there was significantly less
sea ice in the Arctic Ocean, probably less than 50 % of the summer 2007
coverage, which is absolutely lowest on record.
Progress in understanding this connection has converged on two key factors: (1) the variability of autumn snow cover in Eurasia, and (2) the variability of
sea ice coverage in the Barents - Kara Sea during late fall and early wint
sea ice coverage in the Barents - Kara
Sea during late fall and early wint
Sea during late fall and early winter.
BBC News reports that data from Europe's Cryosat spacecraft shows that Arctic
sea ice coverage was nearly 9,000 cubic kilometers (2,100 cubic miles) by the end of this year's melting season, up from about 6,000 cubic kilometers (1,400 cubic miles)
during the same time last year.
Negative delta C - 13 (as) values in glacial AABW were likely caused by poor ventilation
during formation, probably associated with extensive
sea ice coverage.
For the Eastern Fraim Strait, the Southeast Barents
Sea, and North Iceland, there was considerably less sea ice coverage (as assessed in months - per - year) during the late 1600s to early 1700s than there has been during the last few decad
Sea, and North Iceland, there was considerably less
sea ice coverage (as assessed in months - per - year) during the late 1600s to early 1700s than there has been during the last few decad
sea ice coverage (as assessed in months - per - year)
during the late 1600s to early 1700s than there has been
during the last few decades.
(2) Jeff Id's analysis of
sea ice data showed no increase of
ice coverage during the past 30 years.
During the summertime
sea ice melt, after the surface snow has melted off, the albedo of melting
ice is complicated by the presence of melt ponds and depends on the areal
coverage and depth distribution of the melt ponds.