High Temperatures Over Arctic Ocean In June 2018
14
June 2018
It
was 6.6°C
or 44°F (at
850 hPa) over the North Pole due to hot air flowing from Siberia
over the Arctic Ocean on June 13, 2018, 15:00 UTC (left panel).
Earlier, temperatures as high as 7°C or 44.5°F were forecast. At
the same time, the Jet stream (250 hPa) crosses the Arctic Ocean and
goes circular over North Canada and Baffin Bay (right panel).
As the combination image below shows, it was as hot as 32.7°C or 90.9°F (left panel, at the green circle) on June 11, 2018, on the coast of Hudson Bay. The right panel shows the jet stream crossing the Arctic, while numerous cyclones are visible on both images.
The combination image below shows that it was as hot as 30.7°C or 87.3°F (at the green circle, left panel) on the coast of the Laptev Sea, on June 10, 2018. The right panel shows the jet stream crossing the Arctic at speeds as fast as 161 km/h or 100 mph (at the green circle).
There
are three ways in which heat can enter the Arctic Ocean:
1. Heat is reaching the Arctic Ocean through the atmosphere.
2. Furthermore, rivers that end in the Arctic Ocean can carry huge amounts of heat. The image on the right shows that it was as warm as 28.5°C or 83.2°F on May 27, 2018, over the Lena River (at the green circle).
1. Heat is reaching the Arctic Ocean through the atmosphere.
2. Furthermore, rivers that end in the Arctic Ocean can carry huge amounts of heat. The image on the right shows that it was as warm as 28.5°C or 83.2°F on May 27, 2018, over the Lena River (at the green circle).
3.
Heat is also reaching the Arctic Ocean from the Atlantic Ocean and
the Pacific Ocean.
Feedbacks, such as changes to the jet stream can further speed up warming of the Arctic Ocean.
Feedbacks, such as changes to the jet stream can further speed up warming of the Arctic Ocean.
As
the Arctic warms faster than the rest of the world, the temperature
difference between the Arctic and the Equator decreases, the Jet
Stream becomes wavier, with longer loops that allow more warm air to
enter the Arctic and at the same time allow more cold air to flow
out of the Arctic (feedback #10 on the feedbacks
page).
The image on the right shows that the sea surface in the Atlantic Ocean off the coast of North America on May 29, 2018, was as much as 9.8°C or 17.6°F warmer than 1981-2011 (at the green circle).
The image on the right shows that the sea surface in the Atlantic Ocean off the coast of North America on May 29, 2018, was as much as 9.8°C or 17.6°F warmer than 1981-2011 (at the green circle).
As
temperatures keep rising, increasingly stronger winds over oceans
are also causing more heat to enter the Arctic Ocean from the North
Atlantic, and from the Pacific Ocean.
On June 4, 2018, the sea surface in the Pacific Ocean near Bering Strait was as much as 7.2°C or 12.9°F warmer than 1981-2011 (at the green circle), as the second image on the right shows.
As the next image on the right shows, water near Svalbard was as warm as 16.1°C or 61°F on June 4, 2018, versus 3°C or 37.4°F in 1981-2011 (at the green circle).
On June 4, 2018, the sea surface in the Pacific Ocean near Bering Strait was as much as 7.2°C or 12.9°F warmer than 1981-2011 (at the green circle), as the second image on the right shows.
As the next image on the right shows, water near Svalbard was as warm as 16.1°C or 61°F on June 4, 2018, versus 3°C or 37.4°F in 1981-2011 (at the green circle).
On
June 4, 2018, sea surface temperature near Svalbard was as warm as
indicated by the color yellow on the NOAA image, fourth on the
right, i.e. 16-18°C or 60.8-64.4°F.
For
more background on the warm water near Svalbard, also see the
earlier post Accelerating
Warming of the Arctic Ocean.
This heat will warm up the water underneath the sea ice, thus melting the sea ice from below.
Furthermore, as the sea ice retreats, more sunlight will be absorbed by the Arctic Ocean, instead of being reflected back into space, thus further speeding up sea ice decline.
Ocean heat is particularly critical since such a large part of global warming (93.4%) is going into oceans.
This heat will warm up the water underneath the sea ice, thus melting the sea ice from below.
Furthermore, as the sea ice retreats, more sunlight will be absorbed by the Arctic Ocean, instead of being reflected back into space, thus further speeding up sea ice decline.
Ocean heat is particularly critical since such a large part of global warming (93.4%) is going into oceans.
As
the water of the Arctic Ocean keeps warming, the danger increases
that methane hydrates at the bottom of the Arctic Ocean will
destabilize.
Methane releases from the seafloor of the Arctic Ocean can dramatically warm up the atmosphere, especially at higher latitudes.
Ominously, very high methane peaks are increasingly appearing, as high as:
- 2899 ppb on May 04, 2018, a.m.
- 2498 ppb on May 16, 2018, p.m.
- 2820 ppb on May 21, 2018, a.m.
- 2616 ppb on May 22, 2018, p.m.
Methane releases from the seafloor of the Arctic Ocean can dramatically warm up the atmosphere, especially at higher latitudes.
Ominously, very high methane peaks are increasingly appearing, as high as:
- 2899 ppb on May 04, 2018, a.m.
- 2498 ppb on May 16, 2018, p.m.
- 2820 ppb on May 21, 2018, a.m.
- 2616 ppb on May 22, 2018, p.m.
- 3006 ppb on May 27, 2018, p.m.
- 2878 ppb on June 05, 2018, p.m.
- 2605 ppb on June 07, 2018, a.m.
Mean global methane level was as high as 1877 ppb on June 13, 2018, at 254 mb, further confirming that more methane is increasingly accumulating at greater heights in the atmosphere.
NOAA records show that the average May 2018 CO₂ level was 411.25 ppm at Mauna Loa, Hawaii, while the hourly average peaked at well above 416 ppm, as illustrated by the image on the right.
"CO₂ levels are continuing to grow at an all-time record rate because burning of coal, oil, and natural gas have also been at record high levels,” said Pieter Tans, lead scientist of NOAA's Global Greenhouse Gas Reference Network in a news release. "Today's emissions will still be trapping heat in the atmosphere thousands of years from now."
[
click on images to enlarge ]
|
Greenhouse gas levels are particularly high over the Arctic Ocean. CO₂ levels were 420 ppm over the North Pole on June 12, 2018. The situation is getting even more critical as we've left the La Niña period behind and are now moving into an El Niño period, as illustrated by the image on the right.
Given the above, it's amazing that the IPCC in its 'final draft 1.5°C report' insists that "If emissions continue at their present rate, human-induced warming will exceed 1.5°C by around 2040" (according to a recent Reuters report). The final draft is now going to governments for their scrutiny, with the danger that the dire situation may be watered down even further.
Governments
should be urged to confirm that temperatures could rise dramatically
over the next few years. Accordingly, comprehensive and effective
action needs to be taken, as described at the Climate
Plan page.
Links
• Climate Planhttp://arctic-news.blogspot.com/p/climateplan.html
• Feedbackshttp://arctic-news.blogspot.com/p/feedbacks.html
• Accelerating Warming of the Arctic Oceanhttps://arctic-news.blogspot.com/2016/12/accelerating-warming-of-the-arctic-ocean.html
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