J31 Data Workshop 9-10Mar05 Water Vapor during ICARTT 2004: Comparison of AATS-14, J31 in situ, Ron Brown sonde measurements NASA Ames Airborne Sunphotometer.

Slides:



Advertisements
Similar presentations
TAFTS: Atmospheric Profile Uncertainty and Continuum Contribution Ralph Beeby Paul Green, Juliet Pickering 29 th September 2010.
Advertisements

TAFTS: CAVIAR field data from Camborne 2008 Ralph Beeby, Paul Green, Juliet Pickering, John Harries.
Page 1© Crown copyright 2004 Introduction to upper air measurements with radiosondes and other in situ observing systems [3] John Nash, C. Gaffard,R. Smout.
Upper Tropospheric Humidity: A Comparison of Satellite, Radiosonde, Lidar and Aircraft Measurements Satellite Lidar Aircraft Radiosonde.
Psychrometrics.
Lesson 2: Common Sensors and Measurements Systems If only it were this simple!
How do you handle the calculations and data for the gas law lab (molar mass of butane)? February 27.
RADIOSONDE TEMPERATURE, HUMIDITY, AND PRESSURE RESPONSE AT LOW TEMPERATURES Stephen R. Hudson, Michael S. Town, Von P. Walden, and Stephen G. Warren 24.
Are Altitude and Humidity Related? BY SIERRA RITTER.
Humidity. Water Vapor Can make up as little as 1/10 th of 1% to 4% of the atmosphere. Scientists agree that it is the most important atmospheric gas when.
1 Review of WMO test results on the accuracy of radiosonde relative humidity sensors John Nash Observing Methods Technology Centre, Development, Met Office.
Problems and measuring errors of radiosonde humidity measurements in the global aerological network and new possibilities of their correction and validation.
Variability of TTL water vapor A filtered CFH climatology and MLS water vapor for Ticosonde/Costa Rica Rennie Selkirk, NASA GSFC/GESTAR Mark Schoeberl,
European Metrology Research Program (EMRP) MeteoMet Project (October 2011) WP3. Traceable measurements methods and protocols for ground based meteorological.
Radiosondes launched at NSA during the WVIOP04 VAISALA RS90 (operated by ETL and ARM) 4 times per day at the ARM duplex (00, 06, 12, 18 UTC) 1 time per.
Team Philosoraptors: Temperature, Humidity, Pressure Hannah Gardiner Joe Valieant Bill Freeman Randy Dupuis.
Add To Table of Contents:
Infrared Interferometers and Microwave Radiometers Dr. David D. Turner Space Science and Engineering Center University of Wisconsin - Madison
Aerosol Optical Depths from Airborne Sunphotometry in INTEX-B/MILAGRO as a Validation Tool for the Ozone Monitoring Instrument (OMI) on Aura J. Livingston.
PHAT-TACO Experiment On board ACES-23 Hannah Gardiner, Bill Freeman, Randy Dupuis, Corey Myers, Andrea Spring Science Presentation Team Philosohook.
MMS - Ozonesonde Wind and Temperature Comparison during CR-AVE T.P. Bui, J. Dean-Day, C. Chang, R. Castaneda NASA-Ames Research Center H. Voemel University.
Heavier-than-air flight is made possible by a careful balance of four physical forces: lift, drag, weight, and thrust. For flight, an aircraft's lift.
LASE Measurements During IHOP Edward V. Browell, Syed Ismail, Richard A. Ferrare, Susan A Kooi, Anthony Notari, and Carolyn F. Butler NASA Langley Research.
Livingston et al. EGU General Assembly April 2007 Comparison of airborne sunphotometer and satellite sensor retrievals of aerosol optical depth during.
Redemann, ICARTT workshop, Durham, NH, Aug.9-12, 2005 Airborne measurements of spectral direct aerosol radiative forcing - a new aerosol gradient method.
INSTRUMENTATION Introduction to Instrumentation Syarifah Norfaezah
Calculating Relative Humidity Practice Use table from MJ 2006 Paper 1 Q4.
Concept of Humidity What is the relationship between water vapor holding and temperature? Air hold more water vapour at higher temperature.
SRL/Reference sonde P. Di Girolamo, D. Whiteman, B. Demoz, J. Wang, K. Beierle, T. Weckwerth The Reference sonde (C34) consists of a Snow White (SW) chilled-mirror.
AIRS science team meeting Camp Springs, February 2003 Holger Vömel University of Colorado and NOAA/CMDL Upper tropospheric humidity validation measurements.
Height Matters. Wind, Temperature, and Humidity.
VIRTUAL TEMPERATURE T V (Virtual Temp.) is the temperature a dry air parcel would be if its pressure and density were equal to a given moist air sample.
For INTEX-B/MILAGRO the J31 was equipped to measure solar energy and how that energy is affected by atmospheric constituents and Earth's surfaces. Because.
4STAR: Spectrometer for Sky-Scanning, Sun-Tracking Atmospheric Research A collaboration involving: PNNL: Connor J. Flynn, B. Schmid, E. Kassianov NASA.
J31 Data Workshop 9-10Mar05 Validation of Satellite Aerosol Optical Depth by AATS-14 during ICARTT 2004 NASA Ames Airborne Sunphotometer Team Presented.
Vertically resolved aerosol optical properties over the ARM SGP site B. Schmid, H. Jonsson, A. Strawa, B. Provencal, K. Ricci, D. Covert, R. Elleman, W.
IHOP Radiosonde and Dropsonde Data: Highlights and Problems
A new method for first-principles calibration
Three Factors of Weather
1 / 22 Deutscher Wetterdienst Lindenberg Meteorological Observatory Richard Assmann Observatory What final GRUAN observations may consist of and look like.
Aim: What is Humidity and Dew Point? Do Now: What instruments do scientist use to measure air pressure? Explain why in the daytime a breeze comes from.
Cryogenic Hygrometer and Filter Radiometers Ali Aknan Stephanie Vay Melody Avery Jim Plant Charles Hudgins.
Jetstream 31 (J31) in INTEX-B/MILAGRO. Campaign Context: In March 2006, INTEX-B/MILAGRO studied pollution from Mexico City and regional biomass burning,
EMT 462 ELECTRICAL SYSTEM TECHNOLOGY Part 2: Instrumentation By: En. Muhammad Mahyiddin Ramli.
Atmospheric Moisture. Water in the Atmosphere Water vapor is the source of all condensation and precipitation Essentially all water on Earth is conserved.
Airborne Sunphotometry and Closure Studies during the SAFARI-2000 Dry Season Campaign B. Schmid BAER/NASA Ames Research Center, Moffett Field, CA, USA.
Airborne Sunphotometry and Closure Studies in the SAFARI-2000 Dry Season Campaign B. Schmid 1, P.B. Russell 2, P.Pilewskie 2, J. Redemann 1, P.V. Hobbs.
Redemann, ICARTT J-31 data workshop, Boulder, CO, Mar. 9-10, 2005 Aerosol horizontal structure – variability Jens Redemann (BAER Institute) + J-31 team.
Phil Russell 1, John Livingston 2, Beat Schmid 3, Jens Redemann 4, Stephanie Ramirez 4, Qin Zhang 4 and many other contributors 10 Years of Studies Comparing.
Jetstream-31 (J31) in ITCT-INTEX (Intercontinental Transport and Chemical Transformation- Intercontinental Chemical Transport Experiment) J31 GOALS in.
Page 1© Crown copyright 2004 Results of the RS92 Acceptance Test performed by the Met Office (UK) Richard Smout, John Nash, Mark Smees, Darren Lyth, May.
NCAR - Atmospheric Technology Division Reporting work by: Erik Miller (ATD) Junhong Wong (ATD) Ari Paukkunen et al. (Vaisala, OY) Funded by: ATD, Vaisala;
Spectrometer for Sky-Scanning, Sun-Tracking Atmospheric Research (4STAR) Earth Science Division - NASA Ames Research Center 2006 A concept for a sun-sky.
DOE ARM Calibration / Validation Instrumentation Data essentially available in real-time –ARM (Atmospheric Radiation Measurement) –CART (Cloud And Radiation.
Barometry  Evangelista Torricelli credited with invention of barometer.  Gasparo Berti may have been first.
Measurements and modeling of water vapor from solar spectral irradiance during ATTREX Bruce Kindel, Peter Pilewskie, Sebastian Schmidt, Troy Thornberry,
Station lists and bias corrections Jemma Davie, Colin Parrett, Richard Renshaw, Peter Jermey © Crown Copyright 2012 Source: Met Office© Crown copyright.
Introduction to Food Engineering
Expert team on Upper Air System Intercomparisons,
Amanda Williams, Scott Glenn, Josh Kohut,
GAP Measurements and Instrumentation
H2O Sensor Technology.
Assorted Observation Systems
Dew Point and Cloud Formation
For ASME VIII-I vessels, Hydraulic test pressure is
Investigating the T-I annual and semiannual variations in WACCM-X and TIME-GCM using WACCM-X diffusion John T. Emmert(1), Fabrizio Sassi(1), Jennifer Tate(2),
Evaporation Duct Profiles
LT Tom Moneymaker Advisor: Prof Peter Guest
How air temperature affects the speed of sound
BME680 HUMIDITY SENSOR EDDIE SHEA RUCHEN TANG SEAN SWALVE.
Presentation transcript:

J31 Data Workshop 9-10Mar05 Water Vapor during ICARTT 2004: Comparison of AATS-14, J31 in situ, Ron Brown sonde measurements NASA Ames Airborne Sunphotometer Team SSFR Team Presented by John Livingston SRI International

JETSTREAM-31 during ICARTT 2004 Vaisala HMP243 AATS-14 SSFR

HMP243 consists of a heated composite humidity sensor head and an optional sensor head to measure ambient temperature Both probes mounted on the J31 during the ICARTT study Primary output is dewpoint, which is calculated within HMP243 from humidity and temperature readings of composite sensor Separate temp probe permits calculation of ambient relative humidity HMP243 outputs of ambient temperature, T total, and relative humidity, RH Vaisala, were recorded by SSFR data system Because the separate temperature probe is subject to dynamic heating effects, both T total and RH Vaisala must be corrected to account for these effects Calculation of relative humidity by the Vaisala HMP243

Calculation of water vapor density from J31 in-situ measurements Measured quantities: P wing, P nose, T Vaisala probe2, RH Vaisala

P total (wing) P static (nose) Calibration of J31 Pressure Sensors Slide provided by Peter Pilewskie

Calculation of water vapor density from J31 in-situ measurements Measured quantities: P wing, P nose, T Vaisala probe2, RH Vaisala

Table of AATS-14 H 2 O profiles and Ron Brown radiosonde measurements

16 Jul F9

uncorrected

15 Jul F8

22 Jul F13 DC-8 coordination

29 Jul F16

31 Jul F18

2 Aug F20 DC-8 coordination

3 Aug F21 DC-8 coordination

7 Aug F22 DC-8 coordination, MISR

missing sonde?

7 Aug F23