instruments:hatpro:hatpro
Differences
This shows you the differences between two versions of the page.
Both sides previous revisionPrevious revisionNext revision | Previous revisionLast revisionBoth sides next revision | ||
instruments:hatpro:hatpro [2016/06/11 21:14] – susanne | instruments:hatpro:hatpro [2018/07/23 12:51] – andreas | ||
---|---|---|---|
Line 1: | Line 1: | ||
**HATPRO** (//Humidity and Temperature Profiler//) is a microwave radiometer [[http:// | **HATPRO** (//Humidity and Temperature Profiler//) is a microwave radiometer [[http:// | ||
+ | * [[instruments: | ||
* [[instruments: | * [[instruments: | ||
- | * [[instruments: | ||
* [[instruments: | * [[instruments: | ||
+ | * [[instruments: | ||
===== Introduction ===== | ===== Introduction ===== | ||
Line 18: | Line 19: | ||
First developments of microwave radiometer were dedicated to the measurement of radiation of extraterrestrial origin in the 1930s and 1940s [1]. The first operational microwave radiometer was designed by [[https:// | First developments of microwave radiometer were dedicated to the measurement of radiation of extraterrestrial origin in the 1930s and 1940s [1]. The first operational microwave radiometer was designed by [[https:// | ||
- | Soon after satellites were first used for observing the atmosphere, MW radiometers became part of their instrumentation. In 1962 the [[https:// | + | Soon after satellites were first used for observing the atmosphere, MW radiometers became part of their instrumentation. In 1962 the [[https:// |
+ | |||
+ | Ground-Based radiometer for the determination of temperature profiles were first explores | ||
Here we could keep the graphic from the original article | Here we could keep the graphic from the original article | ||
Line 29: | Line 32: | ||
Besides the distinct absorption features of molecular transistion lines, there are also non-resonant contributions by hydrometeors (liquid drops and frozen particles). Liquid water emission increases with frequency, hence, measuring at two frequencies, | Besides the distinct absorption features of molecular transistion lines, there are also non-resonant contributions by hydrometeors (liquid drops and frozen particles). Liquid water emission increases with frequency, hence, measuring at two frequencies, | ||
- | Larger rain drops as well as larger frozen hydrometeors (snow, graupel, hail) also scatter microwave radiation especially at higher frequencies (>90 GHz). These scattering effects can be used to distinguish between rain and cloud water content exploitinh polarized measurements [5] but also to constrain the columnar amount of snow and ice particles from space [6] and from the ground [7]. | + | Larger rain drops as well as larger frozen hydrometeors (snow, graupel, hail) also scatter microwave radiation especially at higher frequencies (>90 GHz). These scattering effects can be used to distinguish between rain and cloud water content exploitinh polarized measurements [9] but also to constrain the columnar amount of snow and ice particles from space [10] and from the ground [11]. |
{{: | {{: | ||
Line 35: | Line 38: | ||
===== Design ===== | ===== Design ===== | ||
- | The principal components of a microwave radiometer | + | A microwave radiometer |
+ | |||
+ | Usually ground-based radiometers are also equipped with environmental sensors (rain, temperature, | ||
- | {{: | + | {{: |
- | Fig. 4: Schematic diagram of a microwave radiometer. | + | Fig. 4: Schematic diagram of a microwave radiometer |
+ | After being received at the antenna the radiofrequency signal is downconverted to the intermediate frequency (IF) with the help of a stable local oscillator signal. After amplification with a Low Noise Amplifier (LNA) and band pass filtering the signal can be detected in full power mode, by splitting or splitting it into multiple frequency bands with a spectrometer. For high-frequency calibrations a Dicke switch is used here. | ||
===== Calibration ===== | ===== Calibration ===== | ||
- | |||
The calibration of MWRs sets the basis for accurate measured TB and therefore, for accurate retrieved atmospheric parameters as temperature profiles, integrated water vapor and liquid water path. The simplest version of a calibation is a so-called „hot-cold“ calibration using two reference blackbodies at known, but different, „hot“ and „cold“ temperatures, | The calibration of MWRs sets the basis for accurate measured TB and therefore, for accurate retrieved atmospheric parameters as temperature profiles, integrated water vapor and liquid water path. The simplest version of a calibation is a so-called „hot-cold“ calibration using two reference blackbodies at known, but different, „hot“ and „cold“ temperatures, | ||
- | The temperatures of the calibration targets should be chosen such that they span the full measurement range. Ground-based radiometers usually use an ambient temperature target as „hot“ reference. As a cold target one can use either a liquid nitrogen cooled blackbody (77 K) [e.g. Ulaby] or a zenith clear sky TB that was obtained indirectly from radiative transfer theory [Paper Westwater]. Satellites use a heated target as „hot“ reference and the cosmic background radiation as „cold“ reference. To increase the accuracy and stabiltity of MWR calibrations further calibration targets, such as internal noise sources, can be used. | + | The temperatures of the calibration targets should be chosen such that they span the full measurement range. Ground-based radiometers usually use an ambient temperature target as „hot“ reference. As a cold target one can use either a liquid nitrogen cooled blackbody (77 K) [1] or a zenith clear sky TB that was obtained indirectly from radiative transfer theory [Paper Westwater]. Satellites use a heated target as „hot“ reference and the cosmic background radiation as „cold“ reference. To increase the accuracy and stabiltity of MWR calibrations further calibration targets, such as internal noise sources, |
===== | ===== | ||
- | |||
The retrieval of physical quantities (e.g. temperature or water vapor profiles) is not straight-forward and comprehensive retrieval algorithms (using inversion techniques like [[https:// | The retrieval of physical quantities (e.g. temperature or water vapor profiles) is not straight-forward and comprehensive retrieval algorithms (using inversion techniques like [[https:// | ||
Line 70: | Line 75: | ||
[2] Thermal Microwave Radiation: Applications for Remote Sensing, C. Matzler, 2006, The Institution of Engineering and Technology, London, Chapter 1. | [2] Thermal Microwave Radiation: Applications for Remote Sensing, C. Matzler, 2006, The Institution of Engineering and Technology, London, Chapter 1. | ||
- | [3] http://cetemps.aquila.infn.it/ | + | [3] Westwater, Edgeworth Rupert, 1970: Ground-Based Determination of Temperature Profiles by Microwaves. PH.D. Thesis, UNIVERSITY OF COLORADO AT BOULDER, Source: Dissertation Abstracts International, |
- | + | ||
[4] Passive Microwave Remote Sensing of the Earth, Physical Foundations, | [4] Passive Microwave Remote Sensing of the Earth, Physical Foundations, | ||
- | [5] Czekala et al. (2001), Discrimination of cloud and rain liquid water path by groundbased polarized microwave radiometry, Geophy. Res. Lett., DOI: 10.1029/ | + | [5] http:// |
+ | |||
+ | [6] Westwater, E.R., C. Mätzler, S. Crewell (2004) A review of surface-based microwave and millimeter-wave radiometric remote sensing of the troposphere. Radio Science Bulletin, No. 3010, September 2004, 59-80, | ||
+ | |||
+ | [7] Westwater, E. R., S. Crewell, C. Mätzler, and D. Cimini, 2006: Principles of Surface-based Microwave and Millimeter wave Radiometric Remote Sensing of the Troposphere, | ||
+ | |||
+ | [8] Final report of the COST action EG-Climet, http:// | ||
+ | |||
+ | [9] Czekala et al. (2001), Discrimination of cloud and rain liquid water path by groundbased polarized microwave radiometry, Geophy. Res. Lett., DOI: 10.1029/ | ||
- | [6] Bennartz, R., and P. Bauer (2003), Sensitivity of microwave radiances at 85–183 GHz to precipitating ice particles, Radio Sci., 38(4), 8075, doi: | + | [10] Bennartz, R., and P. Bauer (2003), Sensitivity of microwave radiances at 85–183 GHz to precipitating ice particles, Radio Sci., 38(4), 8075, doi: |
- | [7| Kneifel et al. (2010), Snow scattering signals in ground-based passive microwave radiometer measurements, | + | [11] Kneifel et al. (2010), Snow scattering signals in ground-based passive microwave radiometer measurements, |
instruments/hatpro/hatpro.txt · Last modified: 2021/01/22 22:17 by 127.0.0.1