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AbsoluteNaturalDisasterRiskIndex

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1D-models suitable for local forecast but problems with advection ... A: High pressure situation, C: cyclonic, X: no advection. A. Glowacka. LCRS 2002 ... – PowerPoint PPT presentation

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Title: AbsoluteNaturalDisasterRiskIndex


1
Understanding of Fog Structure, Development and
Forecasting, COST722
COST 722 member states Austria, Bulgaria,
Cyprus, Finland, France, Germany, Hungary,
Norway, Poland, Spain, Sweden, Switzerland, UK
web page http//www.lcrs.de ? COST presented
by J. Bendix, Faculty of Geography, Laboratory
for Climatology Remote Sensing (LCRS),
University of Marburg, Email bendix_at_staff.uni-mar
burg.de
1. Motivation 2. Main goals and general outline
of COST722 3. Phase 1 results 4. Phase 2
activities within working groups 5. Outlook
14 October 2004, Cape Town, South Africa
2
1. Motivation
Pearson 2002
3
2.1 COST programme major goals
COST Intergovernmental Framework for
European Cooperation in the Field of
Scientific and Technical Research
Hosted by the European Science
Foundation (ESF)
http//cost.cordis.lu/src/whatiscost.cfm
  • co-ordination of nationally funded research
    on a European level
  • ensure that Europe holds a strong position
    in the field of
  • scientific and technical
    research for peaceful purposes
  • cover basic, pre-competitive research and
    activities of public utility
  • increasing European co-operation and
    interaction
  • solving environmental and cross-border
    problems

4
2.2 COST 722
www.lcrs.de
Chairman Dr. Wilfried Jacobs (DWD) Vice
Chairman Vesa Nietosvaara (FMI)
5
2.3 Main objectives
  • Main objective
  • To develop advanced methods for very short-range
    forecasts of fog, visibility
  • and low clouds, adapted to characteristic areas
    and to user requirements
  • This overall objective includes
  • the development of pre-processing methods of
    the necessary input data
  • the development of the appropriate forecast
    models and methods and
  • the development of adaptable application
    software for the production of the forecasts.

6
2.4 Time table
Inventory phase
phase 1 report www.lcrs.de/cost/publications.html
COST-722 Very short range forecasting of fog
and low clouds Inventory phase on current
knowledge and requirements by users and
forecasters, 186 pp.
7
3. Phase 1 results
  • Working Group I Existing forecast methods
    (chair Herbert Gmoser, ZAMG)
  • Conclusions from inventories
  • Intensified use of satellite data for
    nowcasting, better spatio-temporal (3 D) coverage
  • NWP models only reliable for large scale
    forcing
  • 1D-models suitable for local forecast but
    problems with advection
  • Statistical techniques site dependent ? use
    for pre- and postprocessing of model results
  • 3D-models to slow improvements required (e.g.
    microphysics) ? development
  • Working Group II Requirements from the
    forecasters and from the customers
  • (chair Silas
    Michaelides, MSC)
  • Conclusions from questionairs (e.g. aviation
    customers, road authorities)
  • improve short range forecasting quality
  • forecasts should be valid not only for points
    but also for areas of about 20x20 km
  • demand on probability forecasts
  • increased temporal and spatial resolution of
    observation and measurement data is required
  • satellite data with fog channel
  • more information about the climatology of fog
    at more sites

8
4. phase 2 outline and goals
  • Working Group 1 initial data (chair Joerg
    Bendix, PUM-LCRS)
  • provide more sophisticated data on fog (?
    initialization, validation WG 2)
  • provide more detailed climatologies (? tuning of
    statistical methods WG 3)
  • Working Group 2 models (chair Andreas Bott,
    UB-IM)
  • improve models (microphysics, turbulence etc.)
  • Develop cost-effective 3D-models
  • Working Group 3 statistical methods (chair
    Silas Michaelides, MSC)
  • improve statistical methods
  • Develop validation concepts

9
4.1.1 station climatologies and weather situation
A High pressure situation, C cyclonic, X no
advection
A. Glowacka
10
4.1.2 Conceptual models Madrid Airport
red warm advection black catabatic flow
Darío Cano and Enric Terradellas
11
4.1.3 assimilation of satellite data Madrid
Airport
  • estimations of horizontal thermal gradients
    around the airport from Meteosat
  • initialization of the H1D model ? improvement
    of model results by using the
  • catabatic module

Darío Cano and Enric Terradellas
12
4.1.4 Combining SYNOP and satellit data
1961-1990 mean frequency VIS lt 1 km
1989-1999
intermediate maps
13
4.1.5 Combining SYNOP and satellit data
14
4.2.1 1D-model improvement
T. Bergot
15
4.2.2 1D-model performance
False Alarm
Forecast range h
T. Bergot
16
4.2.3 3D-model sensitivity UK Unified Model
12 km
4 km
1 km
Rachel Capon
17
4.2.4 3D-model sensitivity UK Unified Model
12 km
4 km
1 km
Rachel Capon
18
4.3.1 Statistical model for Zurich airport -
predictors
  • Considered predictors
  • Station Data
  • Wind, Wind direction, Temperature, Dewpoint, rel.
    Humidity, Pressure, Net radiative budget
  • On site or very close
  • Precipitation, 5cm Temperature, soil temperature,
    PM10, sun elevation
  • Calculated data (FOGSI fog stability index,
    Inversions, Gradients)
  • Power transformed data (ff, rH, Spread, Q)
  • aLMo NWP Output
  • Several temperature-, wind-, moisture- and
    pressure variables

Meteo Swiss
19
4.3.2 MOS probablistic forecast performance
Good, but biased deterministic forecast
Dijon (winter 2002-2004) Predictors from the
ARPEC model
Y/n
Poor, but unbiased deterministic forecast
Frédéric Atger
YN/(YYYN)
20
5. Outlook
  • improvement of satellite retrievals,
    climatologies and data sets
  • improvement of 1D-models (microphysics,
    turbulence etc.)
  • development of appropriate 3D-applications
    (based on LM, UM etc.)
  • adaptation of statistical models (MOS-based,
    decision trees etc.)
  • intercomparison experiment at Paris CDG
    airport winter 2004/05
  • 1st workshop

http//www.lcrs.de ? COST722
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