Title: AbsoluteNaturalDisasterRiskIndex
1Understanding 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
21. Motivation
Pearson 2002
32.1 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
42.2 COST 722
www.lcrs.de
Chairman Dr. Wilfried Jacobs (DWD) Vice
Chairman Vesa Nietosvaara (FMI)
52.3 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.
62.4 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.
73. 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
84. 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
94.1.1 station climatologies and weather situation
A High pressure situation, C cyclonic, X no
advection
A. Glowacka
104.1.2 Conceptual models Madrid Airport
red warm advection black catabatic flow
DarÃo Cano and Enric Terradellas
114.1.3 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
DarÃo 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
164.2.3 3D-model sensitivity UK Unified Model
12 km
4 km
1 km
Rachel Capon
174.2.4 3D-model sensitivity UK Unified Model
12 km
4 km
1 km
Rachel Capon
184.3.1 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
194.3.2 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)
205. 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