Title: Radar Refractivity Measurements How and Why
1Radar Refractivity Measurements How and Why?
- Jeff Keeler Frédéric Fabry
- NCAR/ATD McGill University
- Boulder, Co Montréal, Canada
2IHOP 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?
3Refractive 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.
4Radar Measurements of Refractive Index
4pf r n c
Target phase ?(r) 2pf ttravel(r)
For fixed targets, phase will change as n changes.
5Convection Regeneration Example
Convective line forms, decays, and reforms on
radar-detected moisture gradient
6S-Pol at IHOP near Liberal, KS
7IHOP 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
8Real Time Display Example
60
Diurnal cycle (mostly)
Wet
Dry
9IHOP Examples Dry-Line Genesis
7º
11º
P3
Broad Td gradient Hints of convergence
10IHOP Examples Dry-Line Genesis
2051
P3
Tight gradient moving
Tightening gradient
11IHOP Examples Dry-Line Evolution
As dry line moves west
To join back after
12On 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
13On N-Field Gradients Without Echoes
Action expected from the west of S-Pol nothing
in the south/east.
14On N-Field Gradients Without Echoes
Insect highway no special meaning
Broad N gradient
South winds as in weather map
15Examples Boundary Layer Processes
Rain accumulation two days before next event
foggy next day
16Examples Boundary Layer Processes
Sunny, cool, calm morning will warm quickly
Anomalous propagation echoes
No wind (!) Maximizes local effects
17IHOP Examples Night-Time Bore
Gust front
18Final Example Initiation Null Case
Moisture gradient on fine line
Three lines of Cu clouds
Moist band
19The evening moisture mismatch mystery
- Evaluate the representativeness and accuracy of
refractivity-derived moisture measurements.
20What 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