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Dr. Christoph Frei Institute for Atmospheric and Climate Science ETH Winterthurerstr. 190 CH-8057 Zuerich |
Tel +41 (0) 1 635 52 32 Fax +41 (0) 1 362 51 97 |
This project aims at deriving spatial analyses and climatological evaluations of precipitation in the region of the European Alps. The project makes use of an unique dataset of rain gauge observations from the high-resolution networks of all Alpine countries. These networks constitute one of the densest meteorological observing systems over complex topography world-wide. The analyses are suitable for research activities on regional climate dynamics, mesoscale meteorology and the evaluation of weather- and climate models.
The project is allocated at the Swiss Federal Institute of Technology Zuerich (ETH, Institute for Atmospheric and Climate Science ETH). The project is closely linked to the Mesoscale Alpine Programme MAP an international research initiative on mesoscale meteorology in the Alpine region.

The climatology is based on an extensive dataset of rain-gauge observations from the operational high-resolution networks of all Alpine countries. The data has been provided by a number of national and regional meteorological and hydrological services. At present a total of about 6700 time series is included with daily observations for at least part of the period 1966-1995. In the average there are about 5000 observations available per day, and this corresponds to a station spacing of 10-15 km. The same region encompasses only about 250 SYNOP stations reporting on the Global Telecomunication System (GTS).
The distribution of stations is fairly balanced over the northern and western portions of the analysis domain, while the coverage is more variable for the southern region. The diagram depicts the station coverage representative for the 20 years 1971-1990. For the more recent years (1991-1995), the station coverage is similar except for northern Italy where the station density is lower than in previous years.
Some of the data supplying institutions have extensively checked the quality of their observations. In other cases only unproofed data was available. For the actual analyses (version 4.0) all daily observations have been passed through a common quality controle procedure, checking for the spatial consistency of the daily reports. Suspect data was then ingnored during the spatial analysis.
Previous versions of the climatology were based on a subset of the rain-gauge database described. A detailed description of the database for version 4.0 is given in Frei and Schär (1998). Check Versions for recent changes in the database.
Mesoscale Alpine precipitation fields are constructed by spatial analysis of quality proofed rain-gauge observations onto a regular grid in geographical latitude and longitude coordinates. The analysis is performed on a daily basis and with a grid resolution of about 25 km.
The applied analysis technique is a modified version of the SYMAP algorithm of Shepard (1968, 1984) and Willmott et al. (1985). It is designed to calculate local area means from a set of station values in the neighbourhood of the analysis grid-points, taking into account the distance and the directional isolation of the station data. The search area is locally adapted to the density of available point observations, resulting in a variable effective spatial resolution. Through this procedure optimal use can be made of high station coverage while still providing a coarser resolution analysis for areas with sparser coverage.
The accuracy of the mesoscale precipitation analysis is influenced by the systematic biases of the rain-gauge measurements and by the limited spatial sampling for the area-mean estimation. Future improvements of the analyses will focus on an extension of the station sample over data-sparse areas and considerations of the non-representative gauge distributions with respect to topography.
A detailed description of the applied analysis scheme, the modifications to the standard procedure and a discussion of the error sources is given in Frei and Schär (1998).
Shepard D.S., 1968: A two-dimensional interpolation function for irregularly-spaced data. Proceedings of 1968 ACM National Conference, 517-524.
Shepard D.S., 1984: Computer mapping: The SYMAP interpolation algorythm. In: Spatial Statistics and Models, (Eds. G.L. Gaile and C.J. Willmott), 133-145.
Willmott C.J., Rowe C.M., Philpot W.D., 1985: Small-scale climate maps: a sensitivity analysis of some common assumptions associated with grid-point interpolation and contouring. The American Cartographer, 12, 5-16.
The actual version 4.0 of the Alpine climatology was released in October 1997 and covers the period 1971-1990. A detailed description of the dataset and analysis method for version 4.0 is given in Frei and Schär (1998) and also includes a climatological analysis over this 20 year reference period. In March 1998 analyses for the recent years (1992-1995) were made accessible. While dense for most regions, this update is based on coarser data over Northern Italy (SYNOP coverage only) however.
Versions of the Alpine precipitation climatology:
| Version Nr. | Date of Release | Changing Characteristics |
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| V4.0 | October 1, 1997 |
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| V3.0 | May 1, 1997 |
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| V2.0 | Jan 1, 1997 |
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| V1.5 | Jan 1, 1996 |
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| V1.0 | July 1, 1995 |
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A number of climatological charts from the actual analyses (V4.0) is available directly in picture format. Select the desired field, month and preferred format to get the chart. These sample fields can also be accessed in digital format (Digital Access).
This site offers access to several products from the latest version (see Versions) of the Alpine Precipitation Climatology in the form of ASCII-files:
| Climatological Fields | Daily Analysis Fields | ||||
|---|---|---|---|---|---|
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* The analyses on these files should be considered as preliminary over Northen Italy (see Interpretation Hints).
The nature of rain-gauge data and the variable density both in time and space require some care in the interpretation of the results of the Alpine precipitation climatology. Here we list some of the most important items, a detailed discussion can be found in Frei and Schär (1998).
Future activities of the project will focus on improvements of the Alpine
precipitation analyses. Further extensions of the current database are sought to
supplement areas and time-periods with currently still week observational basis.
In this respect, high priority is devoted to the compilation of high-resolution
rain gauge data from Northern Italy of the years (1987-1995). An update of the analyses for more recent years is planned but will be
undertaken for bundels of years after major data compilation steps. Activities are currently underway to produce a climatological analysis at
high spatial resolution (a few kilometers) using a more sophisticated analysis
technique that takes account of the statistical relationship of precipitation
with topography. (See Schwarb 2000). Actual efforts are also undertaken to extend the present mesoscale analyses
over the entire 20th century. For this purpose an objective statistical analysis
technique is developed which allows to optimally combine data from a dense
network and limited time period with sparser data for the entire century. These
reconstructions are planned for monthly precipitation on the 25 km grid of the
present analyses. (See Schmidli et al. 2001 and Schmidli 2000). The Alpine rain-gauge dataset is currently exploited with respect to the
daily precipitation statistics aiming at a climatological analysis of heavy
precipitation. The set of mesoscale analyses is also used for the study of the
relationship between regional precipitation and the large-scale dynamical fields
on a day-by-day time scale. The analyses also serve as a reference for
systematic evaluations of mesoscale numerical weather-prediction and climate
models in the Alpine region. Frei C., 1995: An Alpine
precipitation climatology based on high-resolution rain-gauge
observations. MAP Newsletter, No. 3, 46-47. Frei C., and Schär, C., 1997: The frequency of heavy Alpine precipitation
events: Results from the updated rain gauge dataset.
Future Activities
Relevant Publications
MAP Newsletter, No.
7, 46-47.
Frei C., and Schär C., 2001: Detection probability of trends in rare events: Theory and application to heavy precipitation in the Alpine region. J. Climate (in press). [order preprint from Ch. Frei]
Schär C., Davies T., Frei C., Wanner H., Widmann M., Wild M. and Davies H.C., 1998: Current Alpine Climate. In: Cebon P., Dahinden U., Davies H.C., Imboden D., Jäger C. (Eds): A View from the Alps: Regional perspectives on climate change. The MIT press, 21-72.
Widmann M., and Schär C., 1997: A principal component and long-term trend analysis of daily precipitation in Switzerland. Int. J. Climatol., 17, 1-24. [order reprint from Ch. Frei]
Schwarb M., 2000: The Alpine precipitation climate - Evaluation of a high-resolution analysis scheme using comprehensive rain-gauge data. Diss ETH No. 13911.
Schmidli J., 2000: Reconstruction and analysis of mesoscale precipitation in the Alps for the 20th century. Diss ETH No. 13967.
Schmidli J., Frei C., and Schär C., 2001: Reconstruction of mesoscale precipitation fields from sparse observations in complex terrain. J. Climate (in press). [order preprint]
We are indebted to the following institutes for providing access to daily precipitation data: Deutscher Wetterdienst, Offenbach a.M.; Hydrographisches Zentralbüro des Bundesamtes für Land- und Forstwirtschaft, Wien; Zentralanstalt für Meteorologie und Geophysik, Wien; Météo France, Toulouse; MeteoSwiss, Zuerich; Servizio Idrografico e Mareografico Nazionale, Roma; Ufficio Centrale di Ecologia Agraria, Roma; the Italian MAP working group on climatology; Croatian Meteorological and Hydrological Service, Zagreb; Hydrometeorological Institute of Slovenia, Ljubljana.
Send Questions and Comments to Ch. Frei