Gravity Waves – 969628 - #1 The NSF/NCAR G-V Research Aircraft: A New Observing Platform for Environmental Research.

Slides:



Advertisements
Similar presentations
Robin Hogan Julien Delanoe University of Reading Remote sensing of ice clouds from space.
Advertisements

9-10 November 2011 Atmospheric Waves Workshop, ESTEC Atmospheric Waves Workshop Scott Osprey 1, Corwin Wright 2 Evidence of atmospheric gravity waves and.
Lecture 12 Content LIDAR 4/15/2017 GEM 3366.
Thermometer Variable: temperature Units: Degrees Celsius ( o C) Accuracy: marked to 0.5 o C Cost: £10 Site: in the shade (e.g. a Stevenson Screen) Mercury.
PROPOSED FLIGHT PATTERNS. Flow pattern and area of flight operations.
Mountain Waves entering the Stratosphere. Mountain Waves entering the Stratosphere: New aircraft data analysis techniques from T-Rex Ronald B. Smith,
Atmospheric structure from lidar and radar Jens Bösenberg 1.Motivation 2.Layer structure 3.Water vapour profiling 4.Turbulence structure 5.Cloud profiling.
On average TES exhibits a small positive bias in the middle and lower troposphere of less than 15% and a larger negative bias of up to 30% in the upper.
A Global Unmanned Aircraft System (UAS) Observational Network Nikki Priv é August
Boundary Layer Notes 5 Observational Techniques. Sources: Kaimal & Finnegan, Atmospheric Boundary Layer Flows: their structure and measurement, Oxford.
MICROWAVE TEMPERATURE PROFILER (mTP)
The Earth and its Atmosphere This chapter discusses: 1.Gases in Earth's atmosphere 2.Vertical structure of atmospheric pressure & temperature 3.Types of.
SCIENTIST WORK STATIONS Advanced display tools will build on current software to allow for integrated displays of data from onboard instrumentation (e.g.,
July 2001Zanjan, Iran1 Atmospheric Profilers Marc Sarazin (European Southern Observatory)
Application of a High-Pulse-Rate, Low-Pulse-Energy Doppler Lidar for Airborne Pollution Transport Measurement Mike Hardesty 1,4, Sara Tucker 4*,Guy Pearson.
Comparison of temperature data from HIPPO-1 flights using COSMIC profiles and Microwave Temperature Profiler. Kelly Schick 1,2,3 and Julie Haggerty, Ph.D.
Al Cooper Jeff Stith Earth Observing Laboratory (EOL) HIAPER Debrief 9 November 2005 Ongoing Development and Support: EOL Plans for Deployment of HIAPER.
Using GPS data to study the tropical tropopause Bill Randel National Center for Atmospheric Research Boulder, Colorado “You can observe a lot by just watching”
4-d Digital Camera: Horizontal: Horizontal: Large area format Focal Plane detector Arrays Vertical: Vertical: Fourier Transform Spectrometer Time: Time:
Radar Sea Level Pressure Remote Sensing for Improvements in Hurricane Predictions 04 March 2008 Charleston, SC Qilong Min Roland Lawrence Bing Lin, Yongxiang.
Lidar Working Group on Space-Based Winds, Snowmass, Colorado, July 17-21, 2007 A study of range resolution effects on accuracy and precision of velocity.
Page 1© Crown copyright 2004 Cirrus Measurements during the EAQUATE Campaign C. Lee, A.J. Baran, P.N. Francis, M.D. Glew, S.M. Newman and J.P. Taylor.
NARVAL South Lutz Hirsch, Friedhelm Jansen Sensor Synergy While Radars and Lidars provide excellent spatial resolution but only ambiguous information on.
Problems and Future Directions in Remote Sensing of the Ocean and Troposphere Dahai Jeong AMP.
Stephan F.J. De Wekker S. Aulenbach, B. Sacks, D. Schimel, B. Stephens, National Center for Atmospheric Research, Boulder CO; T. Vukicevic,
Water Cycle Breakout Session Attendees: June Wang, Julie Haggerty, Tammy Weckwerth, Steve Nesbitt, Carlos Welsh, Vivek, Kathy Sharpe, Brad Small Two objectives:
GIFTS - The Precursor Geostationary Satellite Component of a Future Earth Observing System GIFTS - The Precursor Geostationary Satellite Component of a.
The Microwave Temperature Profiler (MTP) on START-08 MJ Mahoney - JPL/Caltech Julie Haggerty - NCAR Jan 9, 2008.
Hyperspectral Data Applications: Convection & Turbulence Overview: Application Research for MURI Atmospheric Boundary Layer Turbulence Convective Initiation.
Studies of Emissions & Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys (SEAC 4 RS) Brian Toon Department of Atmospheric and Oceanic.
A NASA / NSF / NRL airborne field campaign focusing on atmospheric composition, chemistry, and climate over Southeast Asia. Programmatic Context, Issues.
Integrating Airborne DWL and PBL Models in Real Time G.D. Emmitt, C. O’Handley, S. A. Wood and S. Greco Simpson Weather Associates WGSBLW Miami 2007.
A fine vertical wave structure & its relation with trace gas transport ATTREX/CONTRAST/CAST Science Team Meeting, Oct, 2014 Ji-Eun Kim University of Colorado,
Flight schedule and staff limitations Hardpoint allocation and cabin layout Time synchronization Flight issues – expectation around convection Sensor groups.
RICO Modeling Studies Group interests RICO data in support of studies.
A NASA / NSF / NRL airborne field campaign focusing on atmospheric composition, chemistry, and climate over Southeast Asia. Programmatic Context, Issues.
Airborne Measurement of Horizontal Wind and Moisture Transport Using Co-deployed Doppler and DIAL lidars Mike Hardesty, Alan Brewer, Brandi McCarty, Christoph.
More on Wind Shear Statistics: Intercomparison of Measurements from Airborne DWL and Ground-based Sensors S. Greco and G.D. Emmitt Simpson Weather Associates.
C. J. Senff, R. J. Alvarez II, R. M. Hardesty, A. O. Langford, R. M. Banta, W. A. Brewer, F. Davies, S. P. Sandberg, R. D. Marchbanks, A. M. Weickmann.
Autonomous Polar Atmospheric Observations John J. Cassano University of Colorado.
Model evolution of a START08 observed tropospheric intrusion Dalon Stone, Kenneth Bowman, Cameron Homeyer - Texas A&M Laura Pan, Simone Tilmes, Doug Kinnison.
SEAC4RS Payload Payload Synergies Synergies. Complementarity between aircraft can be considered to fall into three categories. Each has considerations.
The Deep Convective Clouds and Chemistry (DC3) Field Experiment Mary C. Barth (NCAR), W. H. Brune (PSU), C. A. Cantrell (U. Colorado), S. A. Rutledge (CSU),
Challenges and Strategies for Combined Active/Passive Precipitation Retrievals S. Joseph Munchak 1, W. S. Olson 1,2, M. Grecu 1,3 1: NASA Goddard Space.
Modelling and observations of droplet growth in clouds A Coals 1, A M Blyth 1, J-L Brenguier 2, A M Gadian 1 and W W Grabowski 3 Understanding the detailed.
NOAA Airborne Doppler Update Mike Hardesty, Alan Brewer, Brandi McCarty and Christoph Senff NOAA/ETL and University of Colorado/CIRES Gerhard Ehret, Andreas.
Jetstream 31 (J31) in INTEX-B/MILAGRO. Campaign Context: In March 2006, INTEX-B/MILAGRO studied pollution from Mexico City and regional biomass burning,
Satellites Storm “Since the early 1960s, virtually all areas of the atmospheric sciences have been revolutionized by the development and application of.
Mountain Waves entering the Stratosphere Ronald B. Smith*, Bryan Woods* J. Jensen**, W. Cooper**, J. D. Doyle*** Q. Jiang***, V. Grubisic*** * *Yale University,
Jeff Stith, Andrew Gettelman NCAR is sponsored by the National Science Foundation Southern Ocean Studies: NCAR Measurement capabilities and integrating.
Satellite Indicators of Severe Weather. What Are The Relevant Scientific Questions And Objectives Related To This Topic? Preliminary considerations: Focus.
The identification of the fluctuation effects related to the turbulence and “permanent” layers in the atmosphere of Venus from radio occultation data V.N.Gubenko.
An Outline for Global Precipitation Mission Ground Validation: Building on Lessons Learned from TRMM Sandra Yuter and Robert Houze University of Washington.
Instruments. In Situ In situ instruments measure what is occurring in their immediate proximity. E.g., a thermometer or a wind vane. Remote sensing uses.
METR Introduction to Synoptic Meteorology Other upper air sounding systems, apart from radiosondes University of Oklahoma 2004.
ISTP 2003 September15-19, Airborne Measurement of Horizontal Wind and Moisture Transport Using Co-deployed Doppler and DIAL lidars Mike Hardesty,
The NCAR Microwave Temperature Profiler: Data Applications from Recent Deployments Julie Haggerty, Kelly Schick, Chris Davis National Center for Atmospheric.
Comparison of Temperature Data from HIPPO-1 Flights Using COSMIC and Microwave Temperature Profiler Kelly Schick 1,2,3 and Julie Haggerty 4 1 Monarch High.
The study of cloud and aerosol properties during CalNex using newly developed spectral methods Patrick J. McBride, Samuel LeBlanc, K. Sebastian Schmidt,
Challenges associated with ice and large particles in the TTL
G. Mevi1,2, G. Muscari1, P. P. Bertagnolio1, I. Fiorucci1
G. Mevi1,2, G. Muscari1, P. P. Bertagnolio1, I. Fiorucci1
Upper Troposphere and Lower Stratosphere Break out
NPOESS Airborne Sounder Testbed (NAST)
Group interests RICO data required
Upper Air Data The Atmosphere is 3D and can not be understood or forecast by using surface data alone.
Nonlinear modulation of O3 and CO induced by mountain waves in the UTLS region during TREX Mohamed Moustaoui(1), Alex Mahalov(1), Hector Teitelbaum(2)
Ling Wang and M. Joan Alexander
Group interests RICO data in support of studies
Presentation transcript:

Gravity Waves – #1 The NSF/NCAR G-V Research Aircraft: A New Observing Platform for Environmental Research

Gravity Waves – #2 Other Research Aircraft DC-8 (with MTP) ER2, WB57 HALO (2009?) UK BAe-146 Smaller jets (Learjets, Falcon, etc) Commercial aircraft (esp. in special programs) Turboprop aircraft with wind-sensing (but altitude limitation): –NCAR C-130, P3s, etc. –King Air, Merlin, etc. Many more... but need a quality wind-sensing system

Gravity Waves – #3 G-V Characteristics Certified flight to 51,000 ft; climb to 41,000 ft fully loaded Max. range near 6000 n mi (>10,000 km) 12-person crew; satellite comm. system Wind-sensing: –radome-port system with dual INS/GPS and differential GPS –to be added: all-weather gust system, laser velocimeter, higher-quality INS/GPS

Gravity Waves – #4 Observing Gravity Waves Using Research Aircraft In Situ Measurements: –Wind: horizontal wind vertical wind turbulence characterization –Pressure (including high-resolution for perturbations) –Temperature and air density –Fluxes –Tracers (q, ozone, CO, aerosol conc., etc)

Gravity Waves – #5 Observing Gravity Waves Using Research Aircraft Remote Measurements: –Microwave Temperature Profiler (MTP)-2007 –Aerosol-Backscatter Lidar (HSRL)-2008 –GPS full-spectrum receiver-2008 –Future: Cloud Radar-2009 [Remote sensing of wind] [DIAL lidar(s)]

Gravity Waves – #6 Anticipated Accuracies: Horizontal wind: 0.5 m/s Vertical wind: <0.5 m/s Temperature: 0.3C Pressure: 0.3 mb? MTP: 1-2K, 100 m vertical (for all, resolution is much better so changes of perhaps 10% of these values can be measured reliably)

Gravity Waves – #7 What Capabilities Are New? Altitude and range (and plans for routine operation at UT/LS altitudes) High-quality wind system (with GPS corrections) and flux-measuring system Temperature profiling (soon) Pressure-sensing system capable of measuring pressure fluctuations with high resolution (via differential GPS and special attention to calibration of p measurements)

Gravity Waves – #8 airflow 375K 325K MTP measurements from DC-8 in SOLVE (from MJ Mahoney) p. altitude [km] 10 15

Gravity Waves – #9 GPS Full-Spectrum Receiver Enables the aircraft to perform like a “LEO” satellite: –occultation soundings at locations selected for coverage –ability to measure path-integral time delay in directions of a set of satellites, from above most water vapor –potential uses in conjunction with the MTP

Gravity Waves – #10 GPS

Gravity Waves – #11 Tracers: In addition to the basic parameters of the wave, it is possible to measure many tracers that are steady on the time scale of the wave: –water vapor –ozone –CO –particle concentration –etc.

Gravity Waves – #12 Pressure Measurements Aircraft all measure pressure and fly by reference to a constant pressure Normally, measured pressure fluctuations can't be distinguished from altitude changes GPS systems now provide a high-resolution reference altitude, valid (with diff. GPS) to ca. 10 cm. Opportunity to measure pressure fields with high spatial resolution (from D-value measurements)

Gravity Waves – #13 Measurement Opportunity In a gravity wave, can measure: –fluctuations u',v',w',T',p' (and hence density') –T profiler will provide N and H (or sounding) linear theory constraints these amplitudes, dependent on: k,l,m,N,H,f With all measured except m=vertical wavenumber, have highly constrained solution that provides m, vertical propagation, etc.

Gravity Waves – #14 Example (over Utah)

Gravity Waves – #15 Another Example

Gravity Waves – #16 Polarization Relations Expect vertical and horizontal amplitudes to be similar, and (for typical conditions seen in TREX) p fluctuations to be around 0.5 mb. The corresponding D-value changes are around 20 m, and so are measurable with the combined GPS/pressure system. (approx.)

Gravity Waves – #17 Another Example

Gravity Waves – #18 Variance Spectrum, w

Gravity Waves – #19 Variance Spectrum, w

Gravity Waves – #20 Variance Spectrum, u

Gravity Waves – #21 Observing Opportunities Long ferry legs at UT/LS altitudes provide opportunities for assembling climatology. (Example: TREX flown from Colorado, ferry legs to California) Aircraft showed good flight characteristics in turbulence (although experience limited) Above-cloud observations possible (and some will be accumulated routinely). Opportunity to characterize turbulence