The Met Office and
Hadley Center don't include Arctic temperatures, where global warming is
happening fastest. Photograph: Jenny E Ross/Corbis
A new paper published in The Quarterly Journal of the Royal Meteorological Society fills in the gaps in the UK Met Office
HadCRUT4 surface temperature data set,
and finds that the global surface warming since 1997 has happened more
than twice as fast as the HadCRUT4 estimate. This short video abstract
summarizes the study's approach and results.
The study, authored by Kevin Cowtan from the University of
York and Robert Way from the University of Ottawa (who both also
contribute to the climate science website
Skeptical Science),
notes that the Met Office data set only covers about 84 percent of the
Earth's surface. There are large gaps in its coverage, mainly in the
Arctic, Antarctica, and Africa, where temperature monitoring stations
are relatively scarce. These are shown in white in the Met Office
figure below. Note the rapid warming trend (red) in the Arctic in the
Cowtan & Way version, missing from the Met Office data set.
Met Office vs. Cowtan & Way (2013) surface temperature coverage and trends
NASA's GISTEMP
surface temperature record tries to address the coverage gap by
extrapolating temperatures in unmeasured regions based on the nearest
measurements. However, the NASA data fails to include corrections for a
change in the way sea surface temperatures are measured - a challenging
problem that has so far only been addressed by the Met Office.
The Berkeley Earth Surface Temperature (
BEST) project used a similar approach as NASA, but with a statistical method known as "
kriging"
to fill in the gaps by interpolating and extrapolating with existing
measurements. However, BEST only applied this method to temperatures
over land, not oceans.
Dr. Cowtan is an interdisciplinary
computational scientist who recognized some potential solutions to this
temperature coverage gap problem.
"Like many
scientists, I'm an obsessive problem solver. Sometimes you see a problem
and think 'That's mine, I can make a contribution here'"
In
their paper, Cowtan & Way apply a kriging approach to fill in the
gaps between surface measurements, but they do so for both land and
oceans. In a second approach, they also take advantage of the
near-global coverage of satellite observations, combining the University
of Alabama at Huntsville (UAH) satellite temperature measurements with
the available surface data to fill in the gaps with a 'hybrid'
temperature data set. They found that the kriging method works best to
estimate temperatures over the oceans, while the hybrid method works
best over land and most importantly sea ice, which accounts for much of
the unobserved region.
Both of their new surface temperature data
sets show significantly more warming over the past 16 years than
HadCRUT4. This is mainly due to HadCRUT4 missing accelerated Arctic
warming, especially since 1997.
Cowtan & Way investigate the
claim of a global surface warming 'pause' over the past 16 years by
examining the trends from 1997 through 2012. While HadCRUT4 only
estimates the surface warming trend at 0.046°C per decade during that
time, and NASA puts it at 0.080°C per decade, the new kriging and hybrid
data sets estimate the trend during this time at 0.11 and 0.12°C per
decade, respectively.
These results indicate that the slowed
warming of average global surface temperature is not as significant as
previously believed. Surface warming has slowed somewhat, in large part
due to
more overall global warming being transferred to the oceans over the past decade.
However, these sorts of temporary surface warming slowdowns (and
speed-ups) occur on a regular basis due to short-term natural
influences.
The results of this study also have bearing on some
recent research. For example, correcting for the recent cool bias
indicates that global surface temperatures are not as far from the
average of climate model projections as we previously thought, and
certainly
fall within the range of individual climate model temperature simulations.
Recent studies that concluded the global climate is a bit less
sensitive to the increased greenhouse effect than previously believed
may also have somewhat underestimated the actual
climate sensitivity.
This is of course just one study, as Dr. Cowtan is quick to note.
"No
difficult scientific problem is ever solved in a single paper. I don't
expect our paper to be the last word on this, but I hope we have
advanced the discussion."
The perceived recent slowdown of global surface temperatures remains an interesting scientific question. It appears to be
due to some combination
of internal factors (more global warming going into the oceans),
external factors (relatively low solar activity and high volcanic
activity), and an underestimate of the actual global surface warming.
How
much each factor is contributing is being investigated by extensive
scientific research, but the Cowtan & Way paper suggests the latter
explanation is a significant contributor. The temporary slowing of
global surface warming appears to be smaller than we currently believe.
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