For more than a hundred years, scientists have known greenhouse
gases warm the atmosphere. But despite trapping more and more heat,
earth's surface temperature over the past decade and a half has
risen slowly. And understanding where the extra heat ends up can be
more complicated.
We talk to Dr Richard Allan, lead researcher on a new project
called Deep-C,
about how the tools to take earth's temperature have changed - and
how new measurements can help scientists investigate what's behind
the surface warming slowdown.
Allan is a
climate science researcher at the University of Reading's
department of meteorology. His career has focussed on combining
measurements with climate models to understand changes in earth's
climate.
Heat sink
When we talk about the earth's temperature, we usually mean the
temperature of the air above the land and ocean, or surface
temperature, as it's what humans experience most directly. But
surface temperature is only a small part of the climate system. In
fact, most of the extra heat the planet absorbs goes into the
oceans. Allan tells us:
"The vast ocean has a huge capacity to
store heat … There's a very good relationship between the extra
radiative energy entering the top of Earth's atmosphere - due to
increases in greenhouse gases - and ocean heating."
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