MAGIC

 Introduction

     Humidity is a highly variable parameter in atmospheric processes and it plays a crucial role in atmospheric motions on a wide range of scales in space and time. Limitations in humidity observation accuracy, as well  as temporal and spatial coverage, often lead to problems in numerical weather prediction, in particular that of clouds and precipitation. Due to these limitations, the verification of humidity simulations in operational weather forecasts and climate modeling are also difficult.

     The emerging ground-based Global Positioning System (GPS) networks present appealing opportunities for  an improved humidity observation source that can help resolve these difficulties. Estimation of the integrated water vapor (IWV) in the atmosphere from the anomalous delays in the radio signals transmitted by the GPS satellites has an accuracy that is at least comparable to that of radiosondes and microwave radiometers, which are presently the primary source of humidity data. In addition, ground-based GPS receivers are portable and economic, providing continuous measurements which are not affected by rain and clouds.

Basic Measurement Principle

     The objective of the MAGIC project is to develop and test the capacity for meteorological organisations to benefit from this new data source, in accord with the CEO objectives of increasing the user base for Earth Observation data.

     There are at least two potential benefits from the GPS observations:

Project Structure

     Three focussed studies of testing and assimilation are  proposed for models at three different spatial and temporal scales:      HIRLAM (HIgh Resolution  Limited-Area Model), is developed in an international cooperation between weather services in Denmark, Finland, France, Iceland, Ireland, the Netherlands, Norway, Spain and Sweden. The Danish Meteorological Institute, which is responsible for operational weather prediction in Denmark and participates in the development and improvement of the HIRLAM system, will participate as a project partner. The current analysis scheme is based on the Optimum Interpolation (OI) method. A preliminary study has revealed some weaknesses in the HIRLAM system where the forecasts tend to become wetter as the forecast length increases. Independent data such as the GPS IWV measurements are needed in order to improve model formulation and parameter tuning. In addition, the GPS data are needed to augment the knowledge of the humidity field by being directly incorporated into the model. However, in the current OI scheme, the GPS data cannot influence the weather forecasts directly. Therefore, a necessary and innovative component of this project is the development of the next generation data assimilation system for HIRLAM. With an enhanced data assimilation system, all HIRLAM members will be able to improve their services.

     The HIRHAM model (HIRLAM dynamics + the Hamburg physics package) has been used at DMI to study the regional climate changes. One of the important aspects in developing the model is the validation. As water vapor is one of the key elements determining the climate, it is essential to simulate it correctly in the climate model. The information provided by the GPS data will help to identify weaknesses in the climate model as it did for the  forecast model.

There are two agencies in Spain interested in the use of GPS integrated water vapor measurements. One is the Instituto Nacional de Meteorologia (INM) , which has institutional responsibility for the meteorological activities in Spain, and is a co-developper of HIRLAM in cooperation with their equivalents in other European countries. Thus the INM has a vested interest in the HIRLAM assimilation system to be developed by the HIRLAM member participating in MAGIC.  The other agency, with a smaller geographical scope, is the Servei de  Meteorologia de Catalunya (SMC). This organisation is concerned with the prediction of catastrophic rainfall events for the Catalonian region, due to storm systems unique to the western Mediterranean that are difficult to predict with the operational  (larger scale) numerical weather prediction models. Such storm events are often associated with flash floods with loss of property, and in some cases, human casualties. The SMC is a user of the outputs from a high resolution mesoscale model developed for Catalonia and the surrounding regions, an upgrade of the Mesoscale Atmospheric Simulation System (MASS). While this local model has had some success in predicting precipitation, key humidity data are required to verify the derived humidity fields. For increasing the accuracy of the precipitation estimates, a denser network of water vapor measurements are required than are provided by the conventional global data sources. GPS IWV measurements respond to this need, and also offer a high temporal resolution that ulimately will be of benefit in predicting these rapidly developing storm systems. Assimilation tests for incorporating GPS IWV data into the MASS system or an equivalent mesoscale modeling system for Catalonia will be carried out in the MAGIC project.

    Expected Improvements for the HIRLAM and MASS numerical weather prediction models:

     Expected Improvements for the HIRHAM climate model:      These meteorological agencies at present do not have the expertise nor the infrastructure for retrieving these GPS measurements for a preliminary analysis of their utility. A large number of permanent GPS stations have been installed in Europe, and more are in the process of being installed, to support geodetic and geodynamic research. In bringing together the latest developments in techniques from the space geodetic and meteorological communities, the MAGIC project will be instrumental in making a significant advance in weather prediction and climate modeling. This contributes directly to the objectives of the CEO programme by expanding the customer base of this type of Earth Observation data to the meteorological community. Through CEO enabling services and the European Wide Service Exchange EWSE, the results of the project and example data sets suitable for validation tests will be made available to other potential customers and expand the use of this EO data to a larger group of  meteorological agencies and climate researchers.
 
 
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Page last modified 11 November-1998
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