The animation below alternates between 2012 and 2013 ice which is at least 1.5 metres thick. There has been a huge increase in thick ice, and by next spring, most of that region will be more than three metres thick, of thin rotten decayed ice.
Disrupting the Borg is expensive and time consuming!
Google Search
-
Recent Posts
- Grok 3 Trusts The Government
- NPR Climate Experts
- Defending Democracy In Ukraine
- “Siberia might stay livable”
- Deep Thinking From The Atlantic
- Making Up Fake Numbers At CBS News
- Your Tax Dollars At Work
- “experts warn”
- End Of Snow Update
- CBS News Defines Free Speech
- “Experts Warn”
- Consensus Science With Remarkable Precision
- Is New York About To Drown?
- “Anti-science conservatives must be stopped”
- Disappearing New York
- New York To Drown Soon
- “halt steadily increasing climate extremism”
- “LARGE PART OF NORTHERN CALIF ABLAZE”
- Climate Trends In The Congo
- “100% noncarbon energy mix by 2030”
- Understanding The US Government
- Cooling Australia’s Past
- Saving The World From Fossil Fuels
- Propaganda Based Forecasting
- “He Who Must Not Be Named”
Recent Comments
- arn on Defending Democracy In Ukraine
- William on Defending Democracy In Ukraine
- gordon vigurs on “Siberia might stay livable”
- conrad ziefle on NPR Climate Experts
- conrad ziefle on NPR Climate Experts
- conrad ziefle on Defending Democracy In Ukraine
- conrad ziefle on “Siberia might stay livable”
- Timo, not that one! on “Siberia might stay livable”
- arn on Defending Democracy In Ukraine
- arn on “Siberia might stay livable”
No hurricanes, low tornado count, massive ice recover in the Arctic.
2013, the year that alarmists heads exploded trying (and failing) to explain it all away.
Reblogged this on Health Science Watch.
It you draw a line running north from the top of Greenland, through the north pole and extend it to the Siberian coast you can approximate the portion of the ice pack most susceptible to being moved into warm waters by the transpolar drift. The region to the Atlantic side of that line is likely to get routed to the Barents Sea or down the Fram Strait to melt in the Atlantic. The region to the Beaufort Sea side of the line is likely to recirculate in the Beaufort Gyre and thus stick around for a few years. The percentage of MYI on the Gyre side of the ice pack is much greater than any of the post-2006 years and suggests that this rebound from the recent ice area lows has the potential to be a new multi-year trend.