Arctic Sea Ice Maximum Concentrations 1979-2006
- Visualizations by:
- Greg Shirah
- View full credits
Credits
Please give credit for this item to:
NASA/Goddard Space Flight Center Scientific Visualization Studio
Animator
- Greg Shirah (NASA/GSFC) [Lead]
Scientist
- Josefino Comiso (NASA/GSFC)
Datasets used in this visualization
DMSP (Collected with the SSM/I sensor)
Defense Meteorological Satellite Program Special Sensor Microwave Imager
See more visualizations using this data setComiso's Yearly Maximum Sea Ice Concentration
Note: While we identify the data sets used in these visualizations, we do not store any further details nor the data sets themselves on our site.
Related pages
Arctic Sea Ice Maximum - 2016
March 28th, 2016
Read moreAn animation of the Arctic sea ice from September 7th, 2015 through March 24th, 2016 with datesThis video is also available on our YouTube channel. An animation of the Arctic sea ice from September 7th, 2015 through March 24th, 2016 without dates An image of the Arctic sea ice on March 24, 2016. An image of the Arctic sea ice on March 24, 2016 with an orange line showing the 30-year average sea ice extent for the month of March. An image of the Arctic sea ice on March 24, 2016. The 30-year average sea ice extent line for the month of March with transparency matching the above view The date overlay with transparency The maximum Arctic sea ice extent appears to have occurred on March 24, 2016, reaching an extent of 14.52 million square kilometers (5.607 million square miles). This is below the previous lowest maximum recorded in 2015 when it reached 14.54 million square kilometers (5.612 million square miles). Overall, there is a declining trend in the maximum extent of about 2.8 % per decade. This is much smaller than the summer trends, but also reflects the long-term warming trend in the Arctic.While a low maximum gives the extent a head start heading into summer, it turns out that there is not much relation between the maximum and summer minimum and a record low maximum does not portend a record low minimum. This is because the ice near the edge at the time of the maximum is thin, seasonal ice that will melt out early in the summer. The weather conditions in the Arctic during the summer melt season is the most crucial in determining whether a record low is possible in any given year.In this animation, the Arctic sea ice area is derived from a running 3-day maximum of the AMSR2 sea ice concentration where the concentration is greater than 15%. The blueish white color of the sea ice is derived from a 3-day running minimum of the AMSR2 89 GHz brightness temperature that is linearly mapped between the high and low values. Related pages