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GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L03202, doi:10.1029/2003GL018765, 2004
Radiative forcing - measured at Earth’s surface - corroborate the
increasing greenhouse effect
Rolf Philipona,1 Bruno Du¨rr,1 Christoph Marty,1 Atsumu Ohmura,2 and Martin Wild2
Received 3 October 2003; revised 3 December 2003; accepted 23 December 2003; published 6 February 2004.
[1] The Intergovernmental Panel of Climate Change
(IPCC) confirmed concentrations of atmospheric
greenhouse gases and radiative forcing to increase as a
result of human activities. Nevertheless, changes in
radiative forcing related to increasing greenhouse gas
concentrations could not be experimentally detected at
Earth’s surface so far. Here we show that atmospheric
longwave downward radiation significantly increased
(+5.2(2.2) Wm2) partly due to increased cloud amount
(+1.0(2.8) Wm2) over eight years of measurements at eight
radiation stations distributed over the central Alps. Model
calculations show the cloud-free longwave flux increase
(+4.2(1.9) Wm2) to be in due proportion with temperature
(+0.82(0.41) C) and absolute humidity (+0.21(0.10) g m3)
increases, but three times larger than expected from
anthropogenic greenhouse gases. However, after
subtracting for two thirds of temperature and humidity
rises, the increase of cloud-free longwave downward
radiation (+1.8(0.8) Wm2) remains statistically
significant and demonstrates radiative forcing due to an
enhanced greenhouse effect.
Satellite radiation-budget measurements [Raval and
Ramanathan, 1989; Inamdar and Ramanathan, 1997] have
been used to examine the radiative feedbacks in the climate
system. Changes of the Earth’s outgoing longwave radiation
[Harries et al., 2001; Wielicki et al., 2002] have been
reported also from satellite measurements. Yet to our
knowledge, radiative forcing and its direct relation to
surface temperature and humidity changes, has not been
observationally examined in depth and over long time
periods with radiation budget measurements at Earth’s
surface.
[4] Here we present the changes and trends of radiative
fluxes at the surface and their relation to greenhouse gas
increases and temperature and humidity changes measured
from 1995 to 2002 at eight stations of the Alpine Surface
Radiation Budget (ASRB) network.
GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L22208, doi:10.1029/2004GL020937, 2004
Greenhouse forcing outweighs decreasing solar radiation driving rapid
temperature rise over land
Rolf Philipona and Bruno Du¨rr
Physikalisch-Meteorologisches Observatorium Davos, World Radiation Center, Davos Dorf, Switzerland
Received 6 July 2004; revised 1 September 2004; accepted 25 October 2004; published 25 November 2004.
[1] Since 1988, surface temperature over land in Europe
increased three times faster than the northern hemisphere
average. Here we contrast surface climatic and radiative
parameters measured in central Europe over different time
periods, including the extreme summer 2003, to pinpoint
the role of individual radiative forcings in temperature
increases. Interestingly, surface solar radiation rather
decreases since 1981. Also, on an annual basis no net
radiative cooling or warming is observed under changing
cloud amounts. However, high correlation (rT = 0.86) to
increasing temperature is found with total heating radiation
at the surface, and very high correlation (rT = 0.98) with
cloud-free longwave downward radiation. Preponderance of
longwave downward radiative forcing suggests rapidly
increasing greenhouse warming, which outweighs the
decreasing solar radiation measured at the surface and
drives rapid temperature increases over land.
GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L19809, doi:10.1029/2005GL023624, 2005
Anthropogenic greenhouse forcing and strong water vapor feedback
increase temperature in Europe
Rolf Philipona,1 Bruno Du¨rr,2 Atsumu Ohmura,3 and Christian Ruckstuhl3
Received 25 May 2005; revised 8 July 2005; accepted 17 August 2005; published 8 October 2005.
[1] Europe’s temperature increases considerably faster
than the northern hemisphere average. Detailed month-bymonth
analyses show temperature and humidity changes for
individual months that are similar for all Europe, indicating
large-scale weather patterns uniformly influencing
temperature. However, superimposed to these changes a
strong west-east gradient is observed for all months. The
gradual temperature and humidity increases from west to
east are not related to circulation but must be due to
non-uniform water vapour feedback. Surface radiation
measurements in central Europe manifest anthropogenic
greenhouse forcing and strong water vapor feedback,
enhancing the forcing and temperature rise by about a
factor of three. Solar radiation decreases and changing cloud
amounts show small net radiative effects. However, high
correlation of increasing cloud-free longwave downward
radiation with temperature (r = 0.99) and absolute humidity
(r = 0.89), and high correlation between ERA-40 integrated
water vapor and CRU surface temperature changes (r =
0.84), demonstrates greenhouse forcing with strong water
vapor feedback.