The end of weak La Niña, unprecedented Arctic warmth influenced 2012 climate conditions
NOAA, August 6, 2013
The 2012 State of the Climate report is available online.
(Credit: NOAA)
See 15-slide pdf of the presentation here: http://www1.ncdc.noaa.gov/pub/data/cmb/bams-sotc/2012/sotc-2012-webinar-briefing-slides.pdf
“Many of the events that made 2012 such an interesting year are part of the long-term trends we see in a changing and varying climate — carbon levels are climbing, sea levels are rising, Arctic sea ice is melting, and our planet as a whole is becoming a warmer place," said Acting NOAA Administrator Kathryn D. Sullivan, Ph.D. “This annual report is well-researched, well-respected, and well-used; it is a superb example of the timely, actionable climate information that people need from NOAA to help prepare for extremes in our ever-changing environment."
Conditions in the Arctic were a major story of 2012, with the region experiencing unprecedented change and breaking several records. Sea ice shrank to its smallest “summer minimum” extent since satellite records began 34 years ago. In addition, more than 97% of the Greenland ice sheet showed some form of melt during the summer, four times greater than the 1981–2010 average melt extent.
Temperature in 2012 compared to the 1981-2010 average. Credit: NOAA Climate.gov, based on NCDC data. See more.
Highlights:
- Warm temperature trends continue near Earth’s surface:
Four major independent datasets show 2012 was among the 10 warmest
years on record, ranking either 8th or 9th, depending upon the dataset
used. The United States and Argentina had their warmest year on record.
- La Niña dissipates into neutral conditions:
A weak La Niña dissipated during spring 2012 and, for the first time
in several years, neither El Niño nor La Niña, which can dominate
regional weather and climate conditions around the globe, prevailed for
the majority of the year.
- The Arctic continues to warm; sea ice extent reaches record low:
The Arctic continued to warm at about twice the rate compared with
lower latitudes. Minimum Arctic sea ice extent in September and
Northern Hemisphere snow cover extent in June each reached new record
lows. Arctic sea ice minimum extent (1.32 million square miles,
September 16) was the lowest of the satellite era. This is 18 percent
lower than the previous record low extent of 1.61 million square miles
that occurred in 2007 and 54 percent lower than the record high minimum
ice extent of 2.90 million square miles that occurred in 1980. The
temperature of permafrost, or permanently frozen land, reached
record-high values in northernmost Alaska. A new melt extent record
occurred July 11–12 on the Greenland ice sheet when 97 percent of the
ice sheet showed some form of melt, four times greater than the average
melt this time of year.
- Antarctica sea ice extent reaches record high: The
Antarctic maximum sea ice extent reached a record high of 7.51 million
square miles on September 26. This is 0.5 percent higher than the
previous record high extent of 7.47 million square miles that occurred
in 2006 and seven percent higher than the record low maximum sea ice
extent of 6.96 million square miles that occurred in 1986.
- Sea surface temperatures increase: Four
independent datasets indicate that the globally averaged sea surface
temperature for 2012 was among the 11 warmest on record. After
a 30-year period from 1970 to 1999 of rising global sea surface
temperatures, the period 2000–2012 exhibited little trend. Part of this
difference is linked to the prevalence of La Niña-like conditions
during the 21st century, which typically lead to lower global sea
surface temperatures.
- Ocean heat content remains near record levels:
Heat content in the upper 2,300 feet, or a little less than one-half
mile, of the ocean remained near record high levels in 2012. Overall
increases from 2011 to 2012 occurred between depths of 2,300 to 6,600
feet and even in the deep ocean.
- Sea level reaches record high: Following
sharp decreases in global sea level in the first half of 2011 that were
linked to the effects of La Niña, sea levels rebounded to reach record
highs in 2012. Globally, sea level has been increasing at an average
rate of 3.2 ± 0.4 mm per year over the past two decades.
-
Sea ice concentration reached a new record low in mid-September 2012. Credit: NOAA Climate.gov, based on NSIDC data. See more.Ocean salinity trends continue: Continuing a trend that began in 2004, oceans were saltier than average in areas of high evaporation, including the central tropical North Pacific, and fresher than average in areas of high precipitation, including the north central Indian Ocean, suggesting that precipitation is increasing in already rainy areas and evaporation is intensifying in drier locations.
- Tropical cyclones near average: Global
tropical cyclone activity during 2012 was near average, with a total of
84 storms, compared with the 1981–2010 average of 89. Similar to 2010
and 2011, the North Atlantic was the only hurricane basin that
experienced above-normal activity.
- Greenhouse gases climb: Major greenhouse
gas concentrations, including carbon dioxide, methane, and nitrous
oxide, continued to rise during 2012. Following a slight decline in
manmade emissions associated with the global economic downturn, global
CO2 emissions from fossil fuel combustion and cement
production reached a record high in 2011 of 9.5 ± 0.5 petagrams
(1,000,000,000,000,000 grams) of carbon , and a new record of 9.7 ± 0.5
petagrams of carbon is estimated for 2012. Atmospheric CO2
concentrations increased by 2.1 ppm in 2012, reaching a global average
of 392.6 ppm for the year. In spring 2012, for the first time, the
atmospheric CO2 concentration exceeded 400 ppm at several Arctic observational sites.
- Cool temperature trends continue in Earth’s lower stratosphere: The average lower stratospheric temperature, about six to ten miles above the Earth’s surface, for 2012 was record to near-record cold, depending on the dataset. Increasing greenhouse gases and decline of stratospheric ozone tend to cool the stratosphere while warming the planet near-surface layers.
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