a dynamical reconstruction of detailed atmospheric and related regional variability, 1958-2000
DESCRIPTION
A dynamical reconstruction of detailed atmospheric and related regional variability, 1958-2000. Hans von Storch, Frauke Feser, Ralf Weisse, Arnt Pfizenmayer, Katja Woth, Insa Meinke, Mariza Cabral, Charlotte Hagner, Hilmar Messal - PowerPoint PPT PresentationTRANSCRIPT
A dynamical reconstruction of detailed atmospheric and related regional variability, 1958-2000.
Hans von Storch, Frauke Feser, Ralf Weisse, Arnt Pfizenmayer, Katja Woth, Insa Meinke,
Mariza Cabral, Charlotte Hagner, Hilmar MessalInstitute for Coastal Research, GKSS Research Center,
Geesthacht, Germany
Wroclaw, 27. June 2003
a) The basic atmospheric reconstruction; dynamical downscaling, spectral nudging, validation
b) Applications – storms, (waves), lead transport, run-off
c) Scenarios of plausible future change
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Concept of Dynamical DownscalingRCM Physiographic detail
3-d vector of state
Known large scale state
projection of full state on large-scale scale
Large-scale (spectral) nudging
Large scale
Medium scale
Large scale
Medium scale
Spectral nudging vs. standard formulation
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Similarity of zonal wind at 850 hPa between simulations and NCEP re-analyses
large scales
medium scales
Spectral nudging vs. standard formulation
Inst
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Spectral nudging vs. standard formulation
HIPOCAS meeting Madrid Atmospheric fields REMO 5.0 run GKSS Frauke Feser
Mean monthly
precipitation [mm/month]
for 1999.
NCEP REMO
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Spectral nudging vs. standard formulation
Extreme wind speeds
20-year return values of wind speed,
based on daily 1992-97 data (color codes)
plus from station data in NL (numbers in black)
Southern North Sea
DWD REMO
Fese
r, p
ers
. co
mm
.
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Skill in representing marine winds
Red: buoy, yellow: radar, blue: wave model run with REMO winds
wave direction
significant wave height
[days]
[days]
Gerd Gayer, pers. comm., 2001
Lars Bärring, pers. comm., 2003
Estimatedlead emissions(from Pacyna and Pacyna, 2000)
1955
19951955
1975
deposition
Calculated depositions
1995
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model estimate
Analysis REMO simulation difference
Hill
mar
Mess
al,
20
03
Arnt Pfizenmayer, pers. comm., 2003
REMO simulation (forced with NCEP gobal re-analysis)
Precipitation in the Odra catchment
Hillmar Messal, pers. comm.
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“SRES” ScenariosSRES = IPCC Special Report on
Emissions Scenarios
A world of rapid economic growth and rapidintroduction of new and more efficient technology.
A very heterogeneous world with an emphasis onfamily values and local traditions.
A world of “dematerialization” and introduction of clean technologies.
A world with an emphasis on local solutions toeconomic and environmental sustainability.
“ business as usual ” scenario (1992).
A1
A2
B1
B2
IS92a
IPC
C, 2
001
Scenario for changing precipitation in summer at the end of the 21st century
Ch
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hris
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3, n
atu
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Change (%) in
mean summer precipitation total in 99% quantile 5-daily precipitation amounts (rare events)
Ral
f W
eiss
e, 2
003
Win
d statistics, A
2-scenario
for 2070-2100
SM
HI R
CA
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Conclusions
• Multi-decade reconstruction of hourly weather on 50 km grid in all of Europe available, 1958-2002.
• Several aspects checked but far from complete validation. Wind over the sea ok. Broad features of precip, cloudiness ok as well, but other quantities unknown.
• Data (wind, precip, temp ….) may be used to reconstruct various other environmental conditions, such as ocean waves, storm surges, flooding, extreme events, long range transport of matter.
• Data freely available for other research groups.• Polish groups welcome to validate, and use, data in
particular with respect to Polish territory.
Reconstruction of past decades (and longer) regional and local environmental conditions relevant …
• For determination of extreme events (frequency (Poison?), intensity) in terms of weather and impact variables. Preparation of adequate adaptation measures. Minimizing weather related risks.
• Basis of reconstruction of historical climate (transfer functions; proxy data; historical data).
• A posteriori analysis of past political regulations (example: lead, but also: flood protection).
• Determination of range of „normal“ variations, in order to discriminate between natural climate variability and man-made climate change („detection and attribution“).