Thermal and solar radiation errors on air temperature measured with upper-air radiosondes MeteoSwiss R.
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Thermal and solar radiation errors on air temperature measured with upper-air radiosondes
R. Philipona 1 , A. Kräuchi 2 , G. Romanens 1 , G. Levrat 1 , P. Ruppert 3 , E. Brocard 1 , P. Jeannet 1 , D. Ruffieux 1 , B. Calpini 1
1 Federal Office of Meteorology and Climatology MeteoSwiss, CH-1530 Payerne, Switzerland.
2 Institute for Atmospheric and Climate Science, ETH Zurich, CH-8057-Zurich, Switzerland.
3 Meteolabor AG, CH-8620 Wetzikon, Switzerland.
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Motivation
Results from the: WMO Intercomparison of High Quality Radiosonde Systems Yangjiang, China, 12 July - 3 August 2010 Night Day
J. Nash, T. Oakley, H. Vömel, LI Wei, WMO/TD-No. 1580, 2011
Reinvestigation of Meteolabor radiation correction Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Experiments: Atmosphere / Laboratory
1 Measurements of solar and thermal radiation flux profiles through the atmosphere 2 Measurements of the radiation error on unshaded and shaded temperature sensors in flight 3 Measurements of the radiation error on temperature sensors of different diameters in a vacuum chamber
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Radiation Measurements through the Atmosphere
SRS-C34 Radiosondes from Meteolabor and CNR 4 Net Radiometer from Kipp and Zonen
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Radiation Measurements on Radiosondes
Pyranometer and Pyrgeometer measuring downward fluxes Pyranometer and Pyrgeometer measuring upward fluxes
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Solar and Thermal Radiation Fluxes
Satellite Radiation Measurements Solar shortwave Radiation Thermal longwave Rad.
LUR LDR SUR 168 SDR LUR Surface Radiation Measurements LDR
Can we measure radiation profiles through the atmosphere ?
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Longwave Radiation Profiles during the Night
Night flight: 23 Sep 2011, UT21:20
T_n LUR_n LNR_n LDR_n Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Longwave Radiation Profiles during Night and Day
Night flight: 23 Sep 2011, UT21:20 and Day flight: 23 Sep 2011, UT10:13
T_n T_d LUR_n LUR_d LNR_n LNR_d LDR_n LDR_d Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Solar and Thermal Radiation Fluxes
Satellite Radiation Measurements Solar shortwave Radiation Thermal longwave Rad.
SUR SDR LUR LDR SUR 168 SDR LUR Surface Radiation Measurements LDR
Can we measure radiation profiles through the atmosphere ?
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Shortwave and longwave Radiation Profiles
Night flight: 23 Sep 2011, UT21:20 and Day flight: 23 Sep 2011, UT10:13
LUR SUR LDR SDR SDR =+880 W m -2 DIR DIR = 1344 W m -2
LUR_d LUR_n LDR_d LDR_n SUR SDR DIR
Poster – P3(7) Philipona, Kräuchi, Brocard, GRL, 2012 doi:10.1029/2012GL052087
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Longwave Radiation Error during the Night
Night flight: 23 Sep 2011, UT21:20
Longwave Net Radiation on Temperature Sensor Cooling e s
T ^4 LDR LUR LDR
e s
T ^4 LNR
e s
T ^4
T
LUR
Heating
LNR
Cooling Glenn E. Daniels, JAM, 1968: • Reduce sensor Size • Reduce sensor Emissivity • Increase sensor Speed Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Longwave Radiation Error during the Night
WMO China, Night results
Cooling
Meteolabor 50
m
T sensor
Heating Cooling smallest Size uncertain Emissivity same Speed Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Longwave Radiation Error during the Night
WMO China, Night results
Heating Cooling Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss All sensors are too warm All sensors are too cold
Solar Radiation Error during the Day
WMO China, Day results
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Radiation Error during the Day
Day flight: 23 Sep 2011, UT10:13
Total Net Radiation on Temperature Sensor DIR SUR s T ^4 LDR LUR SDR DIR
LDR
e s
T ^4 LNR
e s
T ^4
T
LUR SUR LNR
Longwave Emission Shortwave Absorption e a : (0.05 - 0.3) : (0.01 - 0.2) Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Method to Shade and Unshade -
Aluminium plate (brilliant / black) attached to Meteolabor sonde
-
Temperature sensors on both sides (5cm distance)
-
Alternately one sensor is exposed to the sun
Reference sensor
front view SRS C34
T sensor Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Radiation Error on Meteolabor temperature sensor 50 micron thermocouple temperature sensors unshaded and shaded Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Radiation Error on Temperature Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Radiation Error on Temperature Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Radiation Error measured in Vacuum Chamber 1 Minute on, 1 Minute off Experiment with one Meteolabor sonde having three thermocouple sensors with wires of 20 m , 50 m and 100 m P = 5 hPa v = 5 m/s
Observatory of Lindenberg
Vacuum Chamber Xenon Arc Lamp, Intensity: ~
1650 Wm -2
P = 10 hPa v = 5 m/s P = 30 hPa v = 5 m/s P = 100 hPa v = 5 m/s P = 300 hPa v = 5 m/s Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Radiation Error: Atmosphere / Laboratory Old correction 100 m Lab New correction 50 m Lab 20 m Lab Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Radiation Error Correction during Day
WMO China, Day results
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Summary: Radiation Error Night and Day
Night Day
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss
Summary and Conclusions
WMO China results referenced to new Meteolabor T-correction Night Day
• More night experiments are needed to clarify thermal effects • Future WMO intercomparisons are needed to help improving radiosonde measurements
Thank you for your attention !
Rolf Philipona Federal Office of Meteorology and Climatology MeteoSwiss