Titlebook: Weather Radar; Principles and Advan Peter Meischner Book 2004 Springer-Verlag Berlin Heidelberg 2004 Cloud.Meteorology.Precipitation.Weathe

Intractable

Improved Precipitation Rates and Data Quality by Using Polarimetric Measurements, only the conventional reflectivity (.) and Doppler information are available. In this chapter we emphasise the application in an operational environment with a typical one-degree beam-width radar and a dwell time of about one-sixth of a second, so that it completes a PPI every minute and provides r

ARCH

Decimate

Radar Sensor Synergy for Cloud Studies; Case Study of Water Clouds,ole of non-precipitating clouds in the climate system. High-frequency systems especially, for example, at 35 and 94 GHz, corresponding to about 0.9 and 0.3 cm wavelengths, were exploited for their feasibility to measure the structure of non-precipitating clouds. As a result of several experiments an

goodwill

Assimilation of Radar Data in Numerical Weather Prediction (NWP) Models,ly realised, arises from a combination of developments. NWP models of the European National Meteorological Services (NMS) are now running routinely at the 10 km grid scale and in a few years will be moving to resolutions of the order of 2 km. Such high resolution models require correspondingly high

SIT

Operational Measurement of Precipitation in Cold Climates, floods have dominated both scientific and operational radar meteorology (Atlas, 1990, Collier, 2001). This is natural, as one of the main benefits of weather radars is very dense sampling of precipitating systems in time and space, facilitating real-time warning and nowcasting of mesoscale severe w

慎重

共同給與

Improved Precipitation Rates and Data Quality by Using Polarimetric Measurements, only the conventional reflectivity (.) and Doppler information are available. In this chapter we emphasise the application in an operational environment with a typical one-degree beam-width radar and a dwell time of about one-sixth of a second, so that it completes a PPI every minute and provides r

邊緣帶來墨水

BOLT

Radar Sensor Synergy for Cloud Studies; Case Study of Water Clouds,ole of non-precipitating clouds in the climate system. High-frequency systems especially, for example, at 35 and 94 GHz, corresponding to about 0.9 and 0.3 cm wavelengths, were exploited for their feasibility to measure the structure of non-precipitating clouds. As a result of several experiments an

CLAIM

Assimilation of Radar Data in Numerical Weather Prediction (NWP) Models,ly realised, arises from a combination of developments. NWP models of the European National Meteorological Services (NMS) are now running routinely at the 10 km grid scale and in a few years will be moving to resolutions of the order of 2 km. Such high resolution models require correspondingly high