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An Overview of VTMX Activities at NCAR. David Parsons and William Brown Research Technology Facility/ATD National Center for Atmospheric Research. Initial Questions of Scientific Interest. How do terrain-induced circulations “pattern”

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an overview of vtmx activities at ncar

An Overview of VTMX Activities at NCAR

David Parsons and William Brown

Research Technology Facility/ATD

National Center for Atmospheric Research

slide2

Initial Questions of Scientific Interest

  • How do terrain-induced circulations “pattern”
  • (i.e., where, when and why) mixing and vertical transport in a stable, urban basins?---to bepresented by Dave Parsons
  • 2. How best to measure mixing and vertical transport in stable, urban basins?---wasto be presented by Bill Brown
  • 3. How well do numerical simulations represent these mesoscale circulations and the patterning of mixing and vertical transport? How can simulations be improved?---James Pinto, unable to be here
slide3

Outline

  • Background (Instruments, location, status of data)
  • Generalization of observed terrain induced circulations at our site (Zeroth order findings)
  • Variations in structure of the terrain induced circulations and cold pool generation (1st order findings)
  • Thoughts on where and when mixing and vertical transport occur (Hypotheses to be tested)
  • How best to measure stable cold pool environments, mixing and transport (Pure speculation)
slide4

Location: Just north of the Jordan Narrows

Great Salt Lake

Special thanks to John Horel as this site was selected partly in response to his request about the need to know how much flow enters the Salt Lake Valley from the south

Wasatch Range

RTF

Utah lake

slide5

NCAR Instruments:

  • MAPR – wind profiler
  • Metek Doppler SODAR
  • Two surface stations
  • TAOS -tethersonde (5 levels)
  • Rawinsondes (~2-3 h)
  • SABL (high resolution backscatter lidar)
slide6

Status:

  • Archival and data quality work for the variety sensors is well underway or completed for the six sensor systems. Profiler is the last.
  • Interactive data perusal for data from these sensors can be found at http://www.atd.ucar.edu/sssf/projects/vtmx/
  • Analysis has begun on suspected mixing and transport events and on placing these events within the context of the circulations within the basin
  • Based on the need for improved vertical resolution in stable regions, we are modifying our wind profiler
  • Modeling efforts (MM5) have commenced
slide7

Zeroth Order Findings

1) Well defined nocturnal flow through the gap is a common occurrence during the VTMX IOPs.2) Often the lake breeze arrives in the late afternoon.3) Therefore the southern end of the valley “typically” resides in a very different air mass than the northern portions.

slide8

SODAR Winds: 0000 UTC on 16 Oct.- 0000 18 Oct. Lake Breeze and Nocturnal Drainage Flows

(From H.-J. Kirtzel)

slide9

0th Order (cont.)

4. Lake breeze,

gap flow, canyon

winds, and the

deep dry desert

ABL means

multiple

air masses enter

the basin. Often

not just the same

air mass subject

to changes

in the pressure

gradient.

Dry western ABL

Lake breeze layer

2200 UTC on

8 October

slide10

1100 UTC

9 October

Residual of deep

…western ABL

..of lake breeze

Gap flow

slide11

1st Order Findings

1. The structure and intensity of the flow through the gap varies

(case-to-case and during a case)

2200 UTC 6 Oct. –2200 UTC 7 October

slide14

1st Order Findings

2. Large long wave cooling

rates.

3. Cooling rates can be reduced

by gap flow.

4. Sounding “budgets” might

prove useful.

During 1st Drainage Pulse: Warm, shallow (overshooting) drainage with complex structure aloft

Launch just before 2nd pulse:

Closer match to radiation

with evidence of mixing or

displacements aloft

Observed Radiosonde Cooling Rate vs. Radiative Cooling

(Used Streamer Code (Key, 1996))

where and when does mixing occur
Where and when does mixing occur?
  • Near the top of the gap
  • flow.
slide19

Scanning Aerosol Backscatter Lidar

SABL Data:

0800 –0830 UTC

3 October

where and when does mixing and vertical transport occur
Where and When Does Mixing and Vertical Transport Occur?

2. At the leading

edge of transient

flows (i.e.,

northerly

synoptic surge).

slide21

SODAR measurements

of the impulsive arrival of a

Northerly surge

where and when do mixing and vertical transport occur
Where and When do Mixing and Vertical Transport Occur?

3. Evening

transition is often

a time for wave

activity (low

stability with

shear). Note that

the transition at

this site is when

the lake breeze

transitions to gap

flow.

slide24
SABL

Wave layer at 2 km, period 8m

Clear layer at 1 km

how best to measure terrain induced circulations and vertical transport and mixing
How Best to Measure Terrain Induced Circulations and Vertical Transport and Mixing?
  • Environmental characteristics
    • Dry air masses
    • Light Winds
    • Turbulence is intermittent
    • Night-time conditions
    • Inversions shallow
    • Flows can be shallow
    • Fine-scale structures
    • Clear, cloudy or foggy
profiler and radars
Profiler and Radars
  • There is typically a diurnal cycle in the signal to noise ratio with low ratios at night when turbulence decreases.
  • Signal to noise ratio is relatively poor when conditions are dry.
  • High vertical and temporal resolution is relatively difficult whenever the signal to noise ratio is poor.
  • Seasonal bird migration are a problem at night. We at NCAR learned that the Jordan Narrows efficiently channel the winds, but it also channels birds.
  • Calm winds difficult for spaced antenna techniques.
slide27
MAPR

Multiple Antenna Profiler Radar

  • 915 MHz Wind Profiler
  • Uses spaced antenna techniques
  • Rapid wind measurements
  • (1 – 5 minute winds)
  • Turbulence

Photo: Charlie Martin

slide28
MAPR
  • Observations heavily contaminated with birds
  • Some layers visible before birds
slide29
MAPR
  • Bird algorithm under development and special processing
  • Adapting special processing for our spaced antenna system (Spectral filtering (Merritt SAM), Wavelet filtering
  • (Jordan), and NIMA)
  • Layers clearer
  • More “real” winds
profilers and radars
Profilers and Radars
  • Therefore, VTMX is a very challenging environment for profilers and radars. Some evidence
    • NIMA applications at Shay’s lounge and our struggle with NCAR data
    • “turbulent events visible with radar systems were spare” – UMASS presentation
    • Profiler data “I have problems with it.” – Rich Coulter
  • For next time
    • At NCAR we have purchased a new transmitter, we are going to change our pulse coding to work better with anti-bird alogirthms and we are going to multiple frequency efforts (FDI) to increase vertical resolution
sodar
SODAR
  • Diurnal variation in the signal-to-noise ratio with best signal at night.
  • Light winds and low turbulence are good for acoustic systems.
  • Some evidence of mixing events might be visible in sodar power return, variance and vertical motions.
  • Lessons for NCAR
    • The performance of the METEK sodar exceeded expectations so we just bought one.
    • Try getting winds by tracking acoustic shell (RASS), speed of sound is far from clutter sources (birds, ground clutter, and wire beating etc.)
lidars and soundings
Lidars and soundings
  • GPS soundings do not resolve problems of accurate winds near the surface
    • Lose lock at launch Vaisala is aware of the problem and are trying to fix it
    • LORAN systems gave you winds but just a smooth interpolation
  • Lidars are fantastic (dry and slightly dirty air is good) until the clouds and fog arrive later in winter
conclusions
Conclusions
  • We collected data in stable layers with several instruments with some pleasant surprises:

Truly complex flow in complex terrain, suspect it is hard to accurately predict concentrations in these western urban basins

Frequently observed waves and breaking waves under specific conditions

Large-scale (100s of meters) displacements and mixing common

Pulsing drainage flow

Multiple layering of aersol

Transition periods with waves

Strong winds through the gap with favorable large-scale conditions

Radiative cooling very large and the “budgets” instructive

With a 10-20 C/day cooling rate, large flows needed for shear driven mixing

TAOS was successful in its first field test

SODARs and lidar work well (calm conditions)

what s next
What’s Next
  • Expand detection of mixing and transport events
  • Richardson numbers from tethersondes and sondes to understand the wave and mixing events
  • Understanding the observed variations in the gap flow
  • Understand the differences in predicted versus observed temperature changes (gap flow adds to the mass of the cold pool, but not directly to its intensity?)
  • Become serious about modeling efforts
  • Field work: Next for us at NCAR may be HVAMS due to NSF request for instrumentation, but with instrument upgrades
slide38
SABL

Rapid change in aerosol height

slide39
SABL

More evening transition

slide40
SABL

Morning transition from stable to convective

slide45
MAPR
  • Observes a strong layer about 750 m above ground level.
  • Lowest layers could be ground clutter