Book contents
- Frontmatter
- Contents
- Preface
- Acknowledgments
- 1 An overview of the atmosphere
- 2 The history of radar in atmospheric investigations
- 3 Refractive index of the atmosphere and ionosphere
- 4 Fundamental concepts of radar remote sensing
- 5 Configuration of atmospheric radars – antennas, beam patterns, electronics, and calibration
- 6 Examples of specific atmospheric radar systems
- 7 Derivation of atmospheric parameters
- 8 Digital processing of Doppler radar signals
- 9 Multiple-receiver and multiple-frequency radar techniques
- 10 Extended and miscellaneous applications of atmospheric radars
- 11 Gravity waves and turbulence
- 12 Meteorological phenomena in the lower atmosphere
- 13 Concluding remarks
- Appendix A Turbulent spectra and structure functions
- Appendix B Gain and effective area for a circular aperture
- List of symbols used
- References
- Index
13 - Concluding remarks
Published online by Cambridge University Press: 25 November 2016
- Frontmatter
- Contents
- Preface
- Acknowledgments
- 1 An overview of the atmosphere
- 2 The history of radar in atmospheric investigations
- 3 Refractive index of the atmosphere and ionosphere
- 4 Fundamental concepts of radar remote sensing
- 5 Configuration of atmospheric radars – antennas, beam patterns, electronics, and calibration
- 6 Examples of specific atmospheric radar systems
- 7 Derivation of atmospheric parameters
- 8 Digital processing of Doppler radar signals
- 9 Multiple-receiver and multiple-frequency radar techniques
- 10 Extended and miscellaneous applications of atmospheric radars
- 11 Gravity waves and turbulence
- 12 Meteorological phenomena in the lower atmosphere
- 13 Concluding remarks
- Appendix A Turbulent spectra and structure functions
- Appendix B Gain and effective area for a circular aperture
- List of symbols used
- References
- Index
Summary
Introduction
It should be clear from the foregoing chapters that the range of applications of MST and windprofiler radar is broad and challenging. Some techniques are mature, some are under development, and some are even no doubt yet to be discovered. Measurements of wind velocities and, by extension, wave motions, wave-mean flow interactions, momentum flux deposition and turbulence, are possible. Capabilities for temperature measurements, and the possibility of humidity measurements, have been discussed. Strange echoes such as polar mesosphere summer echoes have given new insights into the plasma processes of the lower thermosphere. Studies of turbulence anisotropy are possible. We have demonstrated functional radar designs that cost as little as $100 000 up to many millions of dollars.
We will not dwell on these many achievements, however, which should be selfevident. What is perhaps of greater interest is the future of these instruments, and this will be the main focus here.
The future
The future harbors both pragmatic and curiosity-driven aspects. From the point of view of the former, networks of radars, providing data for incorporation into computer forecasting and now-casting models, offer the hope of better forecasts. They have been shown to have benefits in forecasting on time-scales from a few hours out to several days, especially with systems deployed in Japan, Europe, and Canada (see Chapter 12). At the time of writing (2015), the European Space Agency is about to launch a specialized satellite instrument (AEOLUS) for measurement of tropospheric winds from space by lidar, and the networks of windprofilers discussed will be crucial tools for validation of these data. However, since the satellite only measures winds at sunrise and sunset, the radars, with their continuous recording capability, will continue to provide valuable input to meteorological models for many years to come.
Accurate records of winds are of course valuable for large-scale forecasts. This can impact aircraft travel, allowing better flight planning. The ability of radars to make reliable measurements of turbulence strengths can also be of value from the perspective of aircraft passenger safety.
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- Chapter
- Information
- Atmospheric RadarApplication and Science of MST Radars in the Earth's Mesosphere, Stratosphere, Troposphere, and Weakly Ionized Regions, pp. 731 - 733Publisher: Cambridge University PressPrint publication year: 2016