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Radar Refractivity Measurements How and Why

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Title: Radar Refractivity Measurements How and Why


1
Radar Refractivity Measurements How and Why?
  • Jeff Keeler Frédéric Fabry
  • NCAR/ATD McGill University
  • Boulder, Co Montréal, Canada

2
IHOP Objectives
  • Science How much does knowing 4-D H2O
    distribution assist in QPF and modeling?
  • Instrumentation How can we best measure H2O,
    especially vapor?
  • S-Pol How accurately can we estimate moisture
    from refractivity measurements?

3
Refractive Index and Meteorology
N Refractivity near the surface N (n 1)
106 where n is the index of refraction N
f(e, T, P) N hence changes as air mass
properties (moisture and temperature) change.
4
Radar Measurements of Refractive Index
4pf r n c
Target phase ?(r) 2pf ttravel(r)
For fixed targets, phase will change as n changes.
5
Convection Regeneration Example
Convective line forms, decays, and reforms on
radar-detected moisture gradient
6
S-Pol at IHOP near Liberal, KS
7
IHOP Ground Targets at S-Pol
Liberal
KS OK
  • Ground targets were plentiful -- many power
    phone lines, elevators, farms,

Hooker
Beaver
Beaver R. valley
Homestead
OK TX
Booker
Perryton
8
Real Time Display Example
60
Diurnal cycle (mostly)
Wet
Dry
9
IHOP Examples Dry-Line Genesis
7º
11º
P3
Broad Td gradient Hints of convergence
10
IHOP Examples Dry-Line Genesis
2051
P3
Tight gradient moving
Tightening gradient
11
IHOP Examples Dry-Line Evolution
As dry line moves west
To join back after
12
On Fine Lines and N-Field Gradients
  • Not all fine lines are visible in refractivity
  • Some convergence regions have little N
    gradients
  • Some convergence lines occur above nocturnal
    stable layer.

Cold front
13
On N-Field Gradients Without Echoes
Action expected from the west of S-Pol nothing
in the south/east.
14
On N-Field Gradients Without Echoes
Insect highway no special meaning
Broad N gradient
South winds as in weather map
15
Examples Boundary Layer Processes
Rain accumulation two days before next event
foggy next day
16
Examples Boundary Layer Processes
Sunny, cool, calm morning will warm quickly
Anomalous propagation echoes
No wind (!) Maximizes local effects
17
IHOP Examples Night-Time Bore
Gust front
18
Final Example Initiation Null Case
Moisture gradient on fine line
Three lines of Cu clouds
Moist band
19
The evening moisture mismatch mystery
  • Evaluate the representativeness and accuracy of
    refractivity-derived moisture measurements.

20
What Next?
  • Evaluate refractivity-derived moisture
    representativeness, accuracy, utility
  • Analysis of the many IHOP events
  • Data assimilation at meso-?/? scale
  • Consider for WSR-88D ORDA product
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