LBA-Claire 2001 Manaus experiment – rawinsoundings Gilberto Fisch (CTA) Paulo Artaxo (USP)

Slides:



Advertisements
Similar presentations
Vaisala GPS station Egyptian Meteorological Authority (EMA) Koubry ELQuobba EMA, Cairo, Egypt, P. BOX : Fax :
Advertisements

© Crown copyright Met Office E-AMDAR evaluation. Mark Smees & Tim Oakley, Met Office, May 2008.
Requirements for monitoring the global tropopause Bill Randel Atmospheric Chemistry Division NCAR.
SWAC – Weather Balloon Launch 24 July 2009 What is a radiosonde What data does it collect Why are those data important.
Vertical Air Motion. Air Parcels Ascend/Descend Adiabatically Expansional CoolingCompressional heating.
Max Oxman. Why is weather forecasting important?  Planning activities  Planting and harvesting crops  Protect livestock  Scheduling flights.
What is a Radiosonde Balloon carries meteorological instruments aloft Temperature, moisture and wind measured at many levels Provides snapshot of these.
September 2008 Weather Observations and Time Zones Val Bennington AOS 101 Val Bennington AOS 101.
Radar Weather Balloon  temperature  winds  air pressure  humidity  precipitation.
Inter-Continental Atmospheric Radiosonde Upper-air Sounding System ( ICARUSS) Hal Cole, Mel Shapiro, Vin Lally, Terry Hock, Rolf Langland Surface & Sounding.
Radiosondes ATS May 5th Balloon Launch. What is a Radiosonde? A radiosonde is a balloon-based instrument platform with radio transmitting capabilities.
Optical Measurements of Aerosols for MIRAGE-MEX University of Iowa Bill Eichinger John Prueger Piotr Lewandowski Heidi Holder.
Intercomparisons of AIRS and NAST retrievals with Dropsondes During P- TOST (Pacific Thorpex Observational System Test) NASA ER-2 NOAA G-IV Dropsonde.
Leah Kos Sara Lavas Lauryn Gonzalez Mentor: Dr. Michael Douglas, NSSL.
Lesson 1 – Earth’s Atmosphere. Air is mostly nitrogen & oxygen. Air is mostly nitrogen & oxygen. Atmosphere is the layers of gas (air) that surround Earth.
Slide 1 Impact of GPS-Based Water Vapor Fields on Mesoscale Model Forecasts (5th Symposium on Integrated Observing Systems, Albuquerque, NM) Jonathan L.
Questions about the PBL 1.What questions should we ask? 2.What are focus characteristics? 3.How would you try to answer these questions in observations?
Lesson 01 Atmospheric Structure n Composition, Extent & Vertical Division.
Guided Notes on the State of the Atmosphere
Xiaoli Zhou, Pavlos Kollias Department of Atmospheric and Oceanic Sciences, McGill University, Montreal, CA.
Stable Atmosphere.
Ch. 8.3 Pressure in Fluids. Pressure pressure – the amount of force applied to a given area – air, just like water, is a fluid (any substance that flows)
Weather Chapter 21 1.
Bauru November 2004 Modelling interpretation of in situ H2O, CH4 and CO2 measured by  SDLA balloon borne instrument (SF2 and SF4 flights). N. Huret(1),G.
Part II: Turbulence Signature and Platform Limitations Dan Weber, Frank W. Gallagher, Ken Howard ©2000 Frank W. Gallagher III.
Gathering Weather Data
Surface Inversions, Atmospheric Stability, and Spray Drift.
The Wind: PGF Pressure gradient force is what sets air in motion
Weather Forecasting & Maps -Meteorologists make forecasts based on models that are produced by supercomputers which perform a large amount of calculations.
Preliminary LES simulations with Méso-NH to investigate water vapor variability during IHOP_2002 F. Couvreux F. Guichard, V.
Gathering Weather Data SWBAT recognize the importance of accurate weather data; describe the technology used to collect weather data; analyze the strengths.
NCAR April 1 st 2003 Mesoscale and Microscale Meteorology Data Assimilation in AMPS Dale Barker S. Rizvi, and M. Duda MMM Division, NCAR
4. It is not very windy today, why is that? 5. Describe 3 different ways to increase the pressure on the air in a balloon. 6. If we traveled to Venus.
16.3 Weather Forecasts.
Gathering Weather Data Section Data From Earth ’ s Surface Meteorologists measure temperature, air pressure, wind speed, and relative humidity __________–
Fire Plume Kinematic Structure Observed Using Doppler Wind Lidar
Height Matters. Wind, Temperature, and Humidity.
METR Introduction to Synoptic Meteorology Other upper air sounding systems, apart from radiosondes University of Oklahoma 2004.
A Case Study of Decoupling in Stratocumulus Xue Zheng MPO, RSMAS 03/26/2008.
Cloud Top Heights of Cumulonimbi, Thermodynamically Estimated from Objective Analysis Data during the Baiu Season Teruyuki KATO ( Meteorological Research.
TAMDAR AERIBAGO Validation Experiments (TAVE) - Memphis Wayne Feltz, Erik Olson, Sarah Bedka, Kristopher Bedka, John Short, Tim Wagner, and Scott Cultice.
W EATHER D ATA & C LIMATE 5 th Grade Science. W EATHER D ATA Meteorologists-are scientists who study weather Meteorologists observe and collect data on.
NCAR - Atmospheric Technology Division Reporting work by: Erik Miller (ATD) Junhong Wong (ATD) Ari Paukkunen et al. (Vaisala, OY) Funded by: ATD, Vaisala;
Weather Observations A meteorologist (mee tee uh RAH luh jist) is a person who studies the weather. Meteorologists take measurements of temperature, air.
U.S. Radiosondes Jan. 2000, NWS awarded contracts to two radiosonde manufacturers, Sippican and InterMet Systems, for the development and submission of.
9/8 Warm Up Review Energy Transfer 1. Which processes of energy/ heat transfers the sun’s energy between particles as well as through empty space? 2.
The Course of Synoptic Meteorology
What are they? What do they do?
What are they? What do they do?
Driftsonde System Capabilities
NAM in D-INSITU Slovenia.
The Atmosphere.
Upper Air Data The Atmosphere is 3D and can not be understood or forecast by using surface data alone.
Representation of the Great Lakes in CRCM5 using 3D ocean model NEMO: impacts on simulated climate Huziy O and Sushama L.
State of the Atmosphere
Questions about the PBL
Changes in the Free Atmosphere
Upper air Meteorological charts
Weather balloons are launched twice a day
Assorted Observation Systems
Predicting the Weather
Upper Air Data The Atmosphere is 3D and can not be understood or forecast by using surface data alone.
Measurements taken on May 7th and 8th By Addison Liming
Characterizing the response of simulated atmospheric boundary layers to stochastic cloud radiative forcing Robert Tardif, Josh Hacker (NCAR Research Applications.
Weather Forecasting.
Weather Day 2 Weather Day 2.
Weather Maps and Forecasting
Predicting the Weather
Predicting the Weather
Meteorological Measurements for Improved Air Quality Modeling
Presentation transcript:

LBA-Claire 2001 Manaus experiment – rawinsoundings Gilberto Fisch (CTA) Paulo Artaxo (USP)

Manaus

Observations - undisturbed tropical forest (Reserva ZF-2 do INPA) - data collected from 2 July until 18 July, 2001 ZF-2

Observations - upper air rawinsounding system (Vaisala Oy, Finland ) with sondes RS80-15G - profiles of air temperature, relative humidity, atmospheric pressure and winds (GPS capabilities)

Balloon with the RS80-15G RS80-15G Radiotransmission 403 MHz Surface reception – Digicora II

Statistics

preliminary results preliminary results

entrainment zone residual layer NBL CBL sunrise noon sunset

July 10, PM sounding

July 11, 2001 soundings

Preliminary results F Well mixed layer developed over forest F height of the CBL around m

Rawinsoundings from forest (high resolution time and vertical space) and from Manaus (twice per day) data available upon request to