Lessons from Mauritius WMO intercomparison and Results of temperature measurement of the aluminized boom sensor of Modem s radiosonde

Similar documents
Results from WMO High Quality Radiosonde Comparison, Mauritius As related to planning Reference Upper Air Observations for GCOS

Observation Development, Met Office, Exeter

Instruments and Methods of Observation Programme, the Report of the President of CIMO. Report to Cg-XV May 2007 Dr. J. Nash President of CIMO

Demonstration of the new InterMet radiosondes system installed at the Tanzania Meterological Agency, Dar-es-Salaam

2 Calculating Biases from Radiosonde Intercomparison Experiments

WORLD METEOROLOGICAL ORGANIZATION. INSTRUMENTS AND OBSERVING METHODS REPORT No. 83

Recent Application of The Accurate Temperature Measuring (ATM) Radiosonde

Overview of Met Office Intercomparison of Vaisala RS92 and RS41 Radiosondes

Report of CoreTemp2017: Intercomparison of dual thermistor radiosonde (DTR) with RS41, RS92 and DFM09 radiosondes

RA III Radiosonde Training Workshop, Buenos Aires, May 2006

Instruments and Methods of Observation Programme

Comparison of Vaisala Radiosondes RS41 and RS92 WHITE PAPER

China BeiDou radiosonde system

W O R L D M E T E O R O L O G I C A L O R G A N I Z A T I O N COMMISSION FOR INSTRUMENTS AND METHODS OF OBSERVATION JOINT

The Meisei sonde data product

WMO INTERNATIONAL RADIOSONDE COMPARISON

PRESENTATIONS ON RECENT NATIONAL TESTS/COMPARISONS. Recent Tests and Comparisons of Radiosonde Operated by Japan Meteorological Agency

Introduction to upper air measurements with radiosondes and other in situ observing systems. John Nash, C. Gaffard,R. Smout and M.

Met Office Intercomparison of Vaisala RS92 and RS41 Radiosondes

GCOS Reference Upper- Air Network

VAISALA RS92 RADIOSONDES OFFER A HIGH LEVEL OF GPS PERFORMANCE WITH A RELIABLE TELEMETRY LINK

WLS70: A NEW COMPACT DOPPLER WIND LIDAR FOR BOUNDARY LAYER DYNAMIC STUDIES.

NEW DEVELOPMENTS AND OPERATIONAL EXPERIENCE WITH UPPER-AIR OBSERVATION TECHNOLOGY

WMO INTERCOMPARISON OF GPS RADIOSONDES

VAISALA RADIOSONDE RS41 COVER IMPROVEMENT

Ground-based temperature and humidity profiling using microwave radiometer retrievals at Sydney Airport.

of Russian demonstrated Fig 1. Russian allowed to the Vektor-M and more difficult. Performance in winter.

Outcomes of a workshop aimed at improved understanding of biases found in analysis of 183 GHz observations

GRUAN Data Flow and RS92 Data Product v2

LUAMI CAMPAIGN FALL 2008 SUMMARY

MEASUREMENT OF UPPER-AIR PRESSURE, TEMPERATURE AND HUMIDITY

A Case Study on Diurnal Boundary Layer Evolution

Change management for the RS92 phase out

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115, D23104, doi: /2010jd014457, 2010

Radiosonde O-B statistics in the stratosphere

The Vaisala Reference Radiosonde Program: First Results and Future Plans

The GRUAN Observing Station Payerne - Switzerland

OPAG on Integrated Observing Systems. Workshop to Improve the Usefulness of Operational Radiosonde Data. (Submitted by the Secretariat)

MEASUREMENTS AND MODELLING OF WATER VAPOUR SPECTROSCOPY IN TROPICAL AND SUB-ARCTIC ATMOSPHERES.

Atmospheric Sounding: Basics, Research and Development Radiosonde, Dropsonde and Driftsonde Junhong (June) Wang NCAR Earth Observing Laboratory

New Radiosonde Temperature Bias Adjustments for Potential NWP Applications Based on GPS RO Data

5.1 Use of the Consensus Reference Concept for Testing Radiosondes. Joe Facundo and Jim Fitzgibbon, Office of Operational Systems,

Exploitation of ground based GPS for Climate and Numerical Weather Prediction applications COST action 716

Transition from VIZ/Sippican to ROTRONIC

Specifications for a Reference Radiosonde for the GCOS Reference. Upper-Air Network (GRUAN)

Barry M. Lesht. Environmental Research Division Argonne National Laboratory Argonne, Illinois 60439

Field experiments at Sodankylä

The GRUAN Observing Station Payerne - Switzerland

Components of uncertainty in measurements by means of AWS

LAUNCH Concept. Lindenberg Observatory

Quality assurance for sensors at the Deutscher Wetterdienst (DWD)

JAMES K. LUERS UNIVERSITY OF DAYTON RESEARCH INSTITUTE ROBERT E. ESKRIDGE NATIONAL CLIMATIC DATA CENTER

Sensitivity of Convective Indices to Humidity Adjustments

DYNAMO/CINDY Sounding Network

Site Report: Lauder, New Zealand

Deutscher Wetterdienst

STATUS OF THE WIGOS DEMONSTRATION PROJECTS

AUTOMATION OF OBSERVING NETWORK IN BMKG

SOME STEP OF QUALITY CONTROL OF UPPER-AIR NETWORK DATA IN CHINA. Zhiqiang Zhao

LAUNCH Concept. Lindenberg Observatory

New Peltier-based chilled-mirror hygrometer SKYDEW

Country Report for Japan (Submitted by Kenji Akaeda, Japan Meteorological Agency)

WMO SPICE. World Meteorological Organization. Solid Precipitation Intercomparison Experiment - Overall results and recommendations

Ryan K. Decker * NASA Marshall Space Flight Center, Huntsville, Alabama. Lee Burns Raytheon, Huntsville, Alabama

Systematic Errors in Global Radiosonde Precipitable Water Data from Comparisons with Ground-Based GPS Measurements

NIWA s Lauder Site 45.0 S, E 370m a.s.l.

The Payerne Meteolabor Radiosonde

Status of GRUAN certification for French sites

Real-World Performance of Temperature Measurements at Automated Weather Stations How well do we do it?

CHAPTER 12. MEASUREMENT OF UPPER-AIR PRESSURE, TEMPERATURE AND HUMIDITY

Vantage Pro Technical Reference

GRUAN management of transition away from RS92 radiosonde summary of developments to date

History & Scope of Remote Sensing FOUNDATIONS

Observations of Integrated Water Vapor and Cloud Liquid Water at SHEBA. James Liljegren

Prospects for radar and lidar cloud assimilation

Observation minus Background Statistics for Humidity and Temperature from Raman lidar, microwave radiometer and COSMO-2

Reference quality upper-air measurements: GRUAN data processing for the Vaisala RS92 radiosonde

MEASUREMENT OF UPPER AIR PRESSURE, TEMPERATURE AND HUMIDITY

Influence of Radiation on the Temperature Sensor Mounted on the Swiss Radiosonde

Model 3024 Albedometer. User s Manual 1165 NATIONAL DRIVE SACRAMENTO, CALIFORNIA WWW. ALLWEATHERINC. COM

Radiation Dry Bias Correction of Vaisala RS92 Humidity Data and Its Impacts on Historical Radiosonde Data

GRUAN Station Report for Ny-Ålesund

SEASONAL AND DAILY TEMPERATURES

GRUAN-wide strategy for the transition away from the RS92 radiosonde

CONTENT 2. ORGANIZATION 3. SERVICES. instruments. (3)Activities of RIC Tsukuba

Comparison of AMSU-B Brightness Temperature with Simulated Brightness Temperature using Global Radiosonde Data

A Comparison of Clear-Sky Emission Models with Data Taken During the 1999 Millimeter-Wave Radiometric Arctic Winter Water Vapor Experiment

Why the Earth has seasons. Why the Earth has seasons 1/20/11

Clear-Air Forward Microwave and Millimeterwave Radiative Transfer Models for Arctic Conditions

W O R L D M E T E O R O L O G I C A L O R G A N I Z A T I O N COMMISSION FOR INSTRUMENTS AND METHODS OF OBSERVATION

RIVAL Field Campaign at the ENA, NSA, & SGP ARM Sites

W 0 R L D M E T E 0 R 0 L 0 G I C A L 0 R G A N I Z A T I 0 N INSTRUMENTS AND OBSERVING METHODS REPORT NO. 40. WMO/TD-No

Assimilation Experiments of One-dimensional Variational Analyses with GPS/MET Refractivity

High-ohmic/high-voltage resistors

Accuracy of Water Vapor Observations from in-situ and Remote Sensing Techniques: First Results from the DEMEVAP 2011 Campaign

GABLS4: an intercomparison of models in extremely stable conditions over Antarctica

Centralized Forecasting Registration and Communication Requirements for Distribution Connected Variable Generators. IESO Training

Stevenson screen temperatures an investigation

The HAMSTRAD Programme at DOME C, Antarctica

TAPM Modelling for Wagerup: Phase 1 CSIRO 2004 Page 41

Transcription:

Lessons from Mauritius WMO intercomparison and Results of temperature measurement of the aluminized boom sensor of Modem s radiosonde Modem participated to the most recent WMO intercomparison of High Quality GPS radiosondes held at Mauritius in February 2005. M2K2 radiosonde was judged to merit the designation of High Quality radiosonde, outlining some remarkable performances and accuracy detailed below: Geopotential height measurement The simultaneous height intercomparisons demonstrated that GPS height measurements gave geopotential heights that were more accurate than the best pressure sensors at all heights above 16 km and were of similar accuracy to pressure sensor measurements at heights below 16 km. Note: MODEM has been using this method, as a pioneer, since 1997. Estimated random error of M2K2 is less than 10 m at most heights

Data Availability During Mauritius comparison, M2K2 data availability percentage was around 98%. Météo-France reporting on acceptance tests performed on each delivery of radiosondes, regularly shows 100% data availability. Temperature measurement Data from Mauritius experimentation have shown a cold bias (-1.0 C) of temperature measurement from M2K2 radiosonde when the following conditions were met simultaneously: o At Night o Above 25 km 35 Systematic differences in nighttime temperature referenced to the average of Graw, Meisei, Sippican, SRS-adjusted and Vaisala WMO High Quality Radiosonde Comparison Test, Mauritius 2005 30 25 Height [km] 20 15 Vaisala RS92 SRS Meisei 10 Modem Sippican 5 Graw 3 Therm SRS-adj 0-2.50-2.00-1.50-1.00-0.50 0.00 0.50 1.00 1.50 Temperature difference [K] This issue has been deeply discussed with CIMO expert, and it has been concluded that it was due to infrared absorption of the white paint coating of M2K2 sensor boom. Since we discovered this problem, MODEM has been working hard on this issue. We have tested a lot of different coatings and solutions. In fact we have to reduce infrared radiation at night without losing the good performance of solar radiation protection provided by the white paint during the day. Finally, we have designed a new sensor boom with the following improvements: o Replacement of the white paint by a varnish coating and vacuum metallization of the boom end o Modification of the boom end shape in order to reduce solar radiation influence close to the temperature sensor

Above improvements give the results presented below: At night Night flight on September 5th 2006 - Chevannes, France : Cold bias between RS92 and M2K2 is shown while M2K2-DC and RS92 are very close. Similar situation for this night flight on May 17 th 2006 Chevannes, France

We can also see on the graphs below that noise due to the balloon pendulum and turbulence around the sensor are better than with the previous boom end shape of the M2K2 Night flight on May 17 th 2006 Chevannes, France Night flight on September 5th 2006 - Chevannes, France

During the day Day flight on September 5th 2006 - Chevannes, France Details Day flight on September 5th 2006 - Chevannes, France During the day, M2K2 et M2K2-DC measurements are similar (less noise with the new boom) and close to RS92

Relative humidity measurement RH measurement from M2K2 were acceptable however there was still room to make improvement. Following the experimentation and according to results, we have brought following changes: o Addition of a second thermistor under the cap o Different positioning of the cap allowing a better ventilation of the sensor Daylight At Night Comparison of air temperature against temperature measured under the cap During daylight flight, air temperature and temperature under the cap is significantly different. Thus, it is preferable to take into account the actual temperature close to the RH sensor (under the cap) in the calculation of relative humidity, even if this parameter has only a small influence on the result.

Daylight At Night Humidity corrected with temperature measured under the cap ADDITIONAL TESTS After our own tests, M2K2-DC is presently deeply tested by Meteo-France in the scope of an international tendering procedure. Results and official report would be available early 2007. According to CIMO recommendation, it is also scheduled to evaluate the M2K2-DC at Camborne, the UK Met- Office s test station.