Geen diatitel - ECA&D

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On the use of indices to study
changes in climate extremes
EGS-AGU-EUG Joint Assembly
Nice, France, 10 April 2003
Albert Klein Tank
KNMI, the Netherlands
Guide
1. How do we define extreme events?
2. Extremes in daily precipitation and temperature series
from weather stations
3. Observed trends in Europe, 1946-now

“amplified” response of very wet days

“asymmetric” warming of cold & warm tail
!
www.cred.be
WMO status of global climate in 2002
www.wmo.ch
www.dwd.de/research/gpcc/
Day-count indices of extremes
www.knmi.nl/samenw/eca/
Day-count indices of extremes
www.knmi.nl/samenw/eca/
Day-count indices of extremes
Relation between relative trend bq/X required for 80%
detection probability (5% level) and series length N
for extreme events with average return period Tret
bq X ~  Tret 365 1 2
bq X ~ N 3 2
3x
6x
Klein Tank and Können, J. Climate (accepted)
“Amplified” response of very wet days
Linear trends in rainy season, last ~50 years
Easterling et al. (BAMS, 2000) in IPCC-TAR
Precipitation fraction due to very wet days “R95%tot”
1) Identify very wet days using
a site specific threshold = 95th
percentile at wet days in the
1961-90 period
2) Determine fraction of total
precipitation in each year that is
due to these days
3) Trend analysis in series of fractions
www.knmi.nl/samenw/eca/
Frich et al. (Clim. Res., 2002) in IPCC-TAR
Trends 1961-2001
APN 2002 (Della-Marta, Haylock et al.) www.bom.gov.au/bmrc/csr/apn/
Caribbean workshop, Jamaica 2001 (Peterson et al., 2002, JGR)
Trends in 5-day rainfall total 1961-1990
Africa workshop, Casablanca 2001
European precipitation trends



Averaged over Europe, all indices of wet extremes
saw increases between 1946-1999, although spatial
trend coherence is low and many station trends are
not significant
The index that represents the fraction of the annual
amount due to very wet days gives a signal of
disproportionate large changes in the extremes
IPCC-TAR:

“2 to 4% increase in frequency of heavy events in
mid- and high latitudes of the NH”

“in regions where total precipitation has increased
... even more pronounced increases in heavy
precipitation events”
IPCC-TAR, Ch.2, Folland and Karl
upper 10-ptile
1961-1990
the year 1996
lower 10-ptile
1961-1990
upper 10-ptile
1961-1990
the year 1996
lower 10-ptile
1961-1990
“cold
nights”
“warm
nights”
upper 10-ptile
1961-1990
the year 1996
lower 10-ptile
1961-1990
“cold
nights”
www.knmi.nl/samenw/eca/
www.knmi.nl/samenw/eca/
www.knmi.nl/samenw/eca/
European temperature trends



Recent trends (1946-1999) in temperature extremes
reflect the general warming: fewer cold extremes,
more warm extremes
Averaged over all stations, the first decades of slight
cooling saw narrowing of temperature distributions,
whereas the last decades of strong warming saw
widening of temperature distributions
IPCC-TAR:

“lengthening of the freeze-free season in most
mid- and high latitude regions”

“reduction in frequency of extreme low monthly
and seasonal average temperatures and smaller
increase in frequency of extreme high average
temperatures”
ECA&D website: www.knmi.nl/samenw/eca

questions…?
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