Figure 4a. Explore current and archived sea ice data on the NSIDC Sea Ice Index Web site. Many areas, such as the Beaufort and Chukchi Seas, Canada Basin, and Baffin Bay, had lower sea surface temperatures at this time relative to August. The linear downward trend in 4+ year old ice extent at the sea ice minimum is 70,000 square kilometers (27,000 square miles) per year, equivalent to a decline of 6.1 percent per year relative to the 1984 to 2020 average. The 1981 to 2010 median is in dark gray. 2017. Researchers Walt Meier, Ted Scambos, Mark Serreze, and Julienne Stroeve regularly contribute to ASINA, sometimes featuring guest authors, and with support from Kevin Beam, Andy Barrett, Lisa Booker, Michael Brandt, Florence Fetterer, Matt Fisher, Agnieszka Gautier, Marin Klinger, Jonathan Kovarik, Jed Lenetsky, Luis Espinosa Lopez, Audrey Payne, Bruce Raup, Matt Savoie, Trey Stafford, Bruce Wallin, and Ann Windnagel. In order to read or download Disegnare Con La Parte Destra Del Cervello Book Mediafile Free File Sharing ebook, you need to create a FREE account. Ten days after the minimum extent was reached, the total extent climbed above 4 million square kilometers (1.54 million square miles) and by the end of the month the ice extent was tracking at 4.25 million square kilometers (1.64 million square miles), still second lowest in terms of daily extent. We have made it easy for you to find a PDF Ebooks without any digging.

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This warmth was primarily observed on the Eurasian side of the Arctic, where air temperatures along the coastal regions of the Laptev Sea reached up to 8 degrees Celsius (14 degrees Fahrenheit) above average. Ice Cream Market Outlook - 2023. © 2019, National Snow and Ice Data Center :: Advancing knowledge of Earth's frozen regions. The magenta line shows the 1981 to 2010 average extent for that month. Scientists blog from Antarctica and provide a glimpse of what it's like to do research in the field. On Thin Ice:Expedition to a Crumbling Ice Shelf.

During the positive phase of the winter AO, there tends to be a pattern of offshore winds along the Russian side of the Arctic, drawing ice out of the Siberian shelf seas (Kara, Laptev, East Siberian, and Chukchi Seas) and causing new ice formation in the openings left behind.

This, combined with low sea level pressure near the pole and over the Kara Sea and Eurasia, spilled cold Arctic air into Eurasia and warm air over Siberia.