Boundary Layer and Dispersion Applications
2nd M ulti-parameter Phased Array Radar Workshop Norman, Oklahoma 18 November 2009
- Dr. Walter D. Bach, Jr.
Environmental Sciences Division Army Research Office walter.d.bach@us.army.mil
Boundary Layer and Dispersion Applications 2 nd M ulti-parameter - - PowerPoint PPT Presentation
Boundary Layer and Dispersion Applications 2 nd M ulti-parameter Phased Array Radar Workshop Norman, Oklahoma 18 November 2009 Dr. Walter D. Bach, Jr. Environmental Sciences Division Army Research Office walter.d.bach@us.army.mil Outline
2nd M ulti-parameter Phased Array Radar Workshop Norman, Oklahoma 18 November 2009
Environmental Sciences Division Army Research Office walter.d.bach@us.army.mil
– M P
AR
– NRC Report : From the Ground Up – OFCM J
AG/ Atmospheric Transport And Diffusion
– Real time Severe Weather – Nowcast Airport Wind
Hazards
– Enroute ice and turbulence – Heavy precipitation – Hydrometeorology – Initialize NWP wind models
and near PBL
– Cooperative – Non-cooperative
– Airborne release of toxins – Spaceflight ops – Ground truth satellites – Fire Weather / Wildland
Fires
– M udslides – Air Quality and Health – Volcanic Ash – Birds as Hazards – Agriculture
NRC O Obs bservations Sup Supporti ting Fundame mental al In Infras astruct cture f for Mes esoscal ale Monitorin ing and and Predic ediction
– T
emperature, moisture, and wind velocity universally required
– M ost requirements below 5 km (deepest PBL) – Smaller scale phenomena need high resolution
– M easurement error – Representativeness error – M odel physics
– Absolute accuracy – Long term
– Research obs are often episodic, ephemeral, and of limited area
tending to focus on details of processes. (They) may fail to contribute reliably or consistently to ongoing operations and therefore could be viewed as untrustworthy, disruptive, or even parasitic.
– Lidar and radar profilers for lower troposphere – 400 – Air Quality Sensors – CO, SO2, O3, 2.5 µm aerosols - 200 in
urban; 175 km rural separation
– Soil moisture and temperature profiles - 3000 – Distributive/ collaborative networks of radar and lidar – GOES based water vapor & temperature profiles in
Continental boundary layer
– Upgrade rail / ground transportation systems to WM O
standards
– Facilitate observational network of Vehicle Infrastructure
Integration initiative
mesoscale observations address BL issues. Few address modeling issues.
separation) adds finer structure to larger scale features through data assimilation, but are too coarse to address BL heterogeniety issues.
designed to work together – within a test bed network concept as recommended by the J AG/ATD and as J AG/JUTB is developing
JAG/ G/ Atmos
pheric T c Transpor
and Diffus usion
R&D &D Strat ategy to y to Meet U t User N r Needs
COORDINATED AGENCY SUPPORT & FUNDING
GOALS
M EASUREM ENT CAP ABILITIES M ODEL EVAL STANDARDS ATD TEST BEDS BRIDGE THE SCALE GAP CAPTURE AND USE EXISTING DATA SETS LOCAL/ REGIONAL M EASUREM ENT SITING Routinely Quantify Uncertainty Interpret Uncertainty
OBJECTIVES
1 mm 1 cm 1 m 10 m 100 m 1 km 10 km 100 km 1000 km
Horizontal grid spacing
CFD
M esoscale
GCM
DNS LES
Building Urban Storm Fronts Synoptic
Physical M odeling
1 mm 1 cm 1 m 10 m 100 m 1 km 10 km 100 km 1000 km
Horizontal grid spacing
M odeling Gap
Rawinsondes
RADAR
Diurnal Boundary Layer
Surface Obs
Building Urban Storm Fronts Synoptic
Surface Layer M eso-Net
ACARS
larger scales
characterize existing measurements
– PBL heights – Stability – Shear – Large rms wind direction error
uncertainty and large effects from small changes (chaotic).
microscale modeling capabilities
Observations M odels Theory
temperature, and moisture at PBL time & space scales (smaller than models)
covering 50 x 50 km footprint continuously.
including urban and coastal environments
Positive
winds
resolution
Negative