July
temperature anomalies in the
Southern Hemisphere
Sam
Carana, via Facebook
The
July temperature anomaly was particularly high on land on the
Southern Hemisphere (1.53°C or 2.75°F, compared to 1901-2000). The
image shows a linear trend over the period 2012-2017.
The
fall in thickness of the sea ice indicates that the buffer has gone
that until now has consumed heat entering the Arctic Ocean during the
melting season. In the absence of this buffer, where can all this
extra heat go?
The
danger is that much of the extra heat will instead reach sediments at
the seafloor of the Arctic Ocean that contain huge amounts of methane
in currently still frozen hydrates.
Higher
temperatures could destabilize methane hydrates, resulting in huge
methane eruptions.
A
polynomial trend, based on NOAA July 1983 to January 2017 global
monthly mean methane data, points at twice as much methane by 2034.
Stronger methane releases from the seafloor could make such a
doubling occur even earlier. Over the next decade, methane will cause
more warming than CO₂ ─ twice as much methane will cause more
than twice as much warming.
From
the post 'Temperature Rise',
at:
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