the_arm_program_network_of_microwave_radiometers_instrumentation_data_and_retrievals1.pdf
TRANSCRIPT
IEEE International Geosciences and Remote Sensing Symposium24-29 July 2011 Vancouver, CA
THE ARM PROGRAM NETWORK OFMICROWAVE RADIOMETERS:
INSTRUMENTATION, DATA, ANDRETRIEVALS
M.P. Cadeddu1 and D.D. Turner2
1Argonne National Laboratory, Argonne, IL 60439, USA2NOAA/National Severe Storms Laboratory, Norman, OK 73072, USA
The number of microwave radiometers wasrecently expanded to cover the frequency range 22
to 183.31 GHz
MWR: 23.8, 31.4 GHz
MWRP: 22 - 59 GHz
MWRHF: 90,150 GHz
GVR: 183.3±1,3,7,14 GHz
GVRP: 170 - 183.3 GHz
Higher frequencies have higher sensitivity toPWV and LWP
0 1 2 3 4 5 6
Brig
htne
ss te
mpe
ratu
re (K
)
PWV (cm)
MWR
200
150
100
50
0
0 1 2 3
183.3±1183.3±3 183.3±7 183.3±14
300
250
200
150
100
50
0
MWRHF
GVRGVRP
tb(c
loud
y) -
tb(c
lear
)
LWP
40
30
20
10
00 20 40 60 80 100
150 9031.423.8
Current RMS Error for the MWR retrievals is ~ 0.5mm for PWV and ~0.25 mm for LWP
Decrease PWV RMSE in the Arctic to less than10% by using the 183 GHz line
Decrease LWP RMSE to ~ 0.10-0.15 mm inall climates by using 90, 150, 170 GHz
…However the higher frequencies presentnew challenges
In the past 4 years 5 TGARS papers were published that usedARM data between 50 and 183 GHz to improve microwavespectroscopy at higher frequencies (1 paper on the 183.3 linewidth [1], 2 papers on the microwave water vapor continuum[2,3], 1 paper on the oxygen line parameters [4], 1 paper onwater dielectric models at [5].)
[1] V. H. Payne, J. S. Delamere, K. E. Cady-Pereira, et al., Air-broadened half-widths of the 22- and 183-GHz water-vapor lines, vol 46, pp 3601-3617, 2008.[2] D. D. Turner, M. P. Cadeddu, U. Lohnert, S. Crewell, A. M. Vogelmann, Modifications to the watervapor continuum in the microwave suggested by ground-based 150-GHz observations, vol. 47, no. 10, pp.3326-3337, 2009.[3] V. H. Payne, E. J. Mlawer K. E. Cady-Pereira J.-L. Moncet, Water Vapor continuum in themicrowave vol 49, vol. 6, pp 2194-2208, 2011.[4] M. P. Cadeddu, V. H. Payne, S. A. Clough, K. Cady-Pereira, and J. C. Liljegren, The effect of theoxygen line-parameter modeling on temperature and humidity retrievals from ground-based microwaveradiometers, vol. 45, no. 7, pp. 2216-2223, 2007.[5] M. P. Cadeddu D. D. Turner , Evaluation of Water Permittivity Models From Ground-BasedObservations of Cold Clouds at Frequencies Between 23 and 170 GHz,DOI:10.1109/TGRS.2011.2121074, 2011.
Radiometers CalibrationAll radiometers that calibrate with tip curves use anautomated calibration algorithm developed within theARM program.
Tip calibration data from 3/11-SGP 30 GHz
Tnd
1. Voltages, calibrationand diagnostic dataare stored in data filesand archived.
2. Cryogenic calibrationrecords are kept in acalibration database
3. All datasets can bereprocessed if needed
The tip calibration algorithm isfully automated with a dynamictracking of the noise diodetemperature and is described inseveral documents.
Days in March 2011
Data Quality Control
Data Quality Office (obvious problems with the data)
Data from the ARM microwave radiometers aresubject to layers of quality control
Data quality flags
Monthly reviews by mentor and monthly qualityreports
Segments of bad data are flagged through DataQuality Reports (DQR)
PWV and LWP Retrievals
PWV and LWP for the MWR at all sites are retrieved with astatistical algorithm seasonally trained with radiosonde data(physical retrievals are available at selected site)
Wide dynamic range: PWV: 0-10 cm Retrieval uncertainty ~0.5 mm PWV LWP: 0-3 mm (3000 g/m2) Retrieval uncertainty 0.25 mm
At the North Slope of Alaska neural network PWVretrievals from the GVR (183 GHz) are available andLWP retrievals are in development
GVR retrievals at the North Slope of AlaskaHigher frequencies (170-183 GHz) are useful in verydry conditions during the Arctic winter (PWV < 5 mm)
New PWV retrievals from theGVR are available
30
20
10
0PW
V e
rror
per
cent
age
%
0 5 10 15 20 25
PWV from radiosondes
LWP retrievals from the GVRand GVRP are in development
0 20 40 60 80 100 0 20 40 60 80 100
15
10
5
0
30
20
10
0
Ret
rieve
d LW
P d
istri
butio
n %
NSA Jan+July 2007
LWP
Temperature and humidity profiles
Statistical retrievals of T and H profiles are available at twoARM sites
Temporal and vertical resolution trade-off Elevated inversions and moisture gradients difficult to resolve
Figure from: J. C. Liljegren, Initial evaluation of profiles of temperature, water vapor, and cloud liquid water from a newmicrowave radiometer, 11th Atmospheric Radiation Measurement (ARM) Program Science Team Meeting, Atlanta, Georgia.,19-23 March 2001.
NSA, PWV~ 0.8 cm
Azores, PWV~1.8 cm
T ( C ) WVd g/m3 RH % -60 -40 -20 - 5 0 1 2 3 0 50 100 200
10
8
6
4
2
0
Hei
ght (
km)
0 50 100 1500 5 10 -50 -30 10 10
Hei
ght (
km)
10
8
6
4
2
0
T ( C ) WVd g/m3 RH %
New generation of 3-channel radiometerswill be deployed in 2011-2012 at all sites
23.8, 30, 89 GHz
Improved stability
Narrower FOV
2 and 3 channelretrievals in development
Gradual replacementof 2-channel MWRs
Data availability
Availability
Algorithm
Retrievals
FrequenciesGHz
Sites
2012-2008-2008-2006-2004-1993-
StatisticalPhysicalPhysicalNeural
NetworkNeural
NetworkStatisticalStatisticalPhysical
PWV*LWP*
PWV*LWP*
PWV*LWP*
PWVA
LWP*
PWVA
LWPA
T&H ProfilesA
PWVA
LWPA
23.8, 30, 8990, 150170-183.3183.3 ±1,3,7,1422-5923.8, 31.4
ALLSGPAMF1NSANSANSA
AMF1ALL
MWR3CMWRHFGVRPGVRMWRPMWR
SummaryThe DOE ARM Climate Research Facility has expanded thenetwork of microwave radiometers to cover frequenciesbetween 22 and 183.3 GHz. All radiometers are consistentlycalibrated and data subject to stringent quality control
The new radiometers were designed to reduce the RMS error ofPWV and LWP retrievals in regions such as the Arctic and inoptically thin clouds
New retrievals involving the use of higher frequencies (90-183GHz) are in development (some are already available) and willsupplement the standard ARM retrievals (23.8 and 31.4 GHz)
Data and retrievals are freely available for download from theARM archives (www.archive.arm.gov)