Intro Corazon : we weten dat methaan en veel grotere capaciteit heeft om warmte vast te houden dan CO2 .Waarom houden de overheden het zo stil of waarom word er zo weinig naar omgekeken ? Want het lijkt erop dat het gehalte methaan sneller blijk te groeien dan het gehalte aan Co 2. Dat verklaard misschien ook waarom we een steeds snellere afname zien van het totale zeeijs op de Noordpool en waarom het zo extreem warm is op de noordpool.
Methane Erupting From Arctic Ocean Seafloor
|57,016 ft||44,690 ft||36,850 ft||30,570 ft||25,544 ft||19,820 ft||14,385 ft||8,368 ft||1,916 ft|
|17,378 m||13,621 m||11,232 m||9,318 m||7,786 m||6,041 m||4,384 m||2,551 m||584 m|
|74 mb||147 mb||218 mb||293 mb||367 mb||469 mb||586 mb||742 mb||945 mb|
The signature of seafloor methane
Above image shows that, over the years, methane levels have risen strongly high in the Troposphere, up into the Stratosphere. This looks like the signature of methane that originated from the seafloor of the Arctic Ocean. The image below further explains why.
The Tropopause separates the Troposphere from the Stratosphere. The Tropophere ends at a height of some 9 km (5.6 mi; 30,000 ft) at the poles, and at a height of some 17 km (11 mi; 56,000 ft) at the Equator.
As said, methane is erupting from the seafloor of the Arctic Ocean concentrated in plumes, unlike methane from wetlands and agriculture that is typically emitted over a wide area. Since seafloor methane is rising in plumes, it hardly shows up on satellite images at lower altitude either, as the methane is very concentrated inside the area of the plume, while little or no increase in methane levels is taking place outside the plume. Since the plume will cover less than half the area of one pixel, such a plume doesn’t show up well at low altitudes on satellite images,
Methane over the Arctic typically does show up on satellite images at altitudes between 4.4 km and 6 km (14,400 ft and 19,800 ft). Seafloor methane will show up better at these higher altitudes where it spreads out over larger areas. At even higher altitudes, methane will then follow the Tropopause, i.e. the methane will rise in altitude while moving closer to the equator.
In conclusion, methane originating from the seafloor of the Arctic Ocean can strongly contribute to high methane levels that show up over the Equator at higher altitudes, but this methane can be misinterpreted for methane originating from tropical wetlands.
Why is methane erupting from the Arctic Ocean?
Why are increasingly large quantities of methane erupting from the seafloor of the Arctic Ocean? The main driver is warming of the Arctic Ocean that is destabilizing once-permanently-frozen sediments that contain huge amounts of methane in the form of hydrates and free gas. Ocean heat is increasingly entering the Arctic Ocean from the Atlantic Ocean, as illustrated by the images below, from earlier posts (see links further below).
Self-reinforcing feedback loops
Meanwhile, Arctic sea ice looks set to take a steep fall, as illustrated by the image below.
The danger is that self-reinforcing feedback loops such as albedo decline and methane releases will further accelerate warming and will, in combination with further warming elements, cause a temperature rise as high as 10°C or 18°F by the year 2026, as described at the extinction page.
The situation is dire and calls for comprehensive and effective action as described in the Climate Plan.
• Low sea ice extent contributes to high methane levels at both poles