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TEFLUN-A Field Experiment in Texas

(based on TEFLUN-A Project Data Catalog by Aaron Tuttle and Edward Zipser ,July, 1998)
TEFLUN-A Overview The TExas and FLorida UNderflights (TEFLUN) Experiment is a mission to obtain validation measurements for the Tropical Rain Measuring Mission (TRMM).TEFLUN-A focused on East Texas is the first in a series of experiments using a combination of airborne and surface-based measurements to complement the satellite data. TEFLUN-A Field Campaign Science Objectives TEFLUN-A goal is to (a)investigate the organization, structure, and evolution of mature convective storms and their interaction with the larger-scale environment and (b) investigate the extent to which the TRMM radar based satellite can be used to infer the vertical structure of clouds as well as other parameters and future applications.

TEFLUN-A Operations The TExas and FLorida UNderflights (TEFLUN) Experiment was conducted from 1 April through 15 May 1998. The project involved six research platforms: the Texas A&M 10-cm wavelength Doppler radar (ADRAD), the NOAA ETL X-band polarization radar and NOAA AL Profiler system, the NASA ER-2 aircraft, the Lear Jet cloud physics aircraft, a Mobile VIZ-GPS Atmospheric Sounding System deployed from TAMU and from the Houston Weather Service Office (WSO). In addition, we archived data from the operational National Weather Service (NWS) WSR-88D network, raingauge clusters, disdrometers

TEFLUN-A was able to launch relatively on schedule. The daily operations were scheduled in a way as prevent anyone from being caught off guard during a convective event across the domain. However, despite proper planning, the atmosphere did not cooperate as hoped. Only a few documentable case studies were obtained during the duration of the project. There were a few equipment problems noted throughout the experiment with the sounding vehicles and the research aircraft. Despite these events, TEFLUN-A can be considered a success as far as planning and preparation goes for such a complicated upscale project.

NASA Aircraft Instruments

During TEFLUN-A , the NASA ER-2 and NASA SPEC Lear Jet cloud physics aircrafts carried instruments relevant to TRMM objectives. ER2-Aircraft Instruments

Primary TRMM-related instruments on the ER-2

ER-2 Doppler Radar (EDOP)

a dual-beam 9.6 GHz Doppler radar that is designed to provide vertical profiles of reflectivity, vertical hydrometeor motions, horizontal winds along the aircraft track, and polarization measurements which provide microphysical information. The EDOP measurements will be used to examine vertical precipitation structure and resolution limitations of the PR.

Advanced Microwave Precipitation Radiometer (AMPR)

, with frequencies similar to TMI (10 - 85 GHz), will provide information on precipitation structure through the rain emission and ice scattering signals.

Lightning Instrument Package (LIP)

designed to provide measurements of the three- dimensional electric field and conductivity. This information will be related to the LIS measurements on the TRMM satellite.

Multispectral Atmospheric Mapping Sounder

(MAMS) with 11 channels visible, near-IR, and IR a 6.7 m moisture channel (similar to that flown on GOES), will provide high resolution visible and infrared ma

Millimeter Imaging Radiometer

(MIR) is a cross-scanning radiometer at frequencies from 90 GHz to 325 GHz.

Other important ER-2 instruments that did fly during TEFLUN-A were

Submillimeter Limb Sounder (SLS)

and

NPOESS Aircraft Sounder Interferometer(NAST-I)

Spec Learjet Cloud Physics Aircraft

Instrumentation:

The basic instrumentation package of Spec Lear Jet cloud physics aircraft measures temperature, dew point temperature, pressure, wind and cloud microphysical characteristics along with aircraft position, attitude and performance parameters. The three dimensional wind field is derived from measurements of acceleration, pitch, roll and yaw combined with angles of attack and sideslip and indicated airspeed. An LTN-76 inertial navigation system and a global positioning system (GPS) supply the aircraft parameters. Turbulence intensity can be derived from differential pressure transducers and accelerometer outputs.

Cloud microphysical measurements are made with an array of Particle Measuring Systems probes (FSSP, 1D-C, 2D-C, 1D-P) mounted on the wing tip pylons. These probes measure concentrations and sizes of particles from one µ to several millimeters in diameter. In addition, there are probes to measure both liquid water content (CSIRO) and icing rate (Rosemount icing meter). For TRMM two new instruments will be available, a Cloud Particle Imager (CPI) and a High Volume Particle Sampler (HVPS), both from SPEC, Inc. These will provide improved resolution above that which is achieved from the PMS probes. The CPI will provide microscopic quality images of small ice particles. The HVPS will replace the 1D-C probe and it will provide improved sample volumn for detection and imaging of large particles. A PMS 2D-P probe may also be used for periods when the HVPS is not available.


Surface Based Facilities
TEFLUN-A Network Surface-based facilities which will form part of the database for TEFLUN-A include the Houston and other WSR-88Ds, the Texas ADRAD Doppler radar, the NOAA ETL X-band polarization radar (X-POL), and the NOAA AL Profiler system. These ground-based facilities are integrated with dense rain gauge networks and disdrometers. Soundings will be obtained from two mobile systems to provide initialization and validation data for models at strategic times and locations.

The TEFLUN-A surface network is shown in the following figure,
please click on image for full size

TEFLUN-A Surface based facilities

The operational mode for surface-based facilities will be contiunous for some and episodic for others. The WSR-88Ds, rain gauges, disdrometers, and profilers will operate continuously. The other surface radars (X-POL in TEFLUN-A) will operate either continuously, or whenever precipitation is within a 150 km range, assuming personnel requirements are met. The mobile soundings will be available to provide data for all significant precipitation systems, all events for which aircraft flights are anticipated, and all TRMM overpasses. Following are the brief operation plan of some of the ground sensors.

  • NOAA/AL Doppler radar profilers

    The NOAA Aeronomy Laboratory will operate two vertically-looking doppler radar profilers for TEFLUN A and B. The two profilers will be colocated and operate at 915 MHz and 2835 MHz, respectively. The profilers are designed to observe precipitation with excellent vertical and temporal resolution. Doppler spectra recorded at each range gate are processed to yield equivalent reflectivity, Doppler velocity and spectral width.

    The primary data product from the profilers are time-height sections of equivalent reflectivity and Doppler velocity. the two collocated profilers facilitate the unambiguous identification of vertical air motion and hydrometeor fall velocities in the Doppler spectra. During TEFLUN-A, the two profilers will be located in South Houston surrounded by a network of rain gauges. Disdrometers will be collocated with the profilers to measure drop-size distributions at the surface.

  • Rain gauge networks & Disdrometers:

    The purpose of the rain gauge and disdrometer deployment during TEFLUN-A is

    • to obtain independent measurements of surface rain rate for calibration and comparison with radar derive estimates in a variety of rainfall regimes and at various ranges from the other radars,
    • to investigate the temporal and spatial variability of rainfall in Texas , and
    • to determine how this variability impacts the accuracy of the ground validation (GV) radar products

    The rain gauges are tipping bucket type (Qualimetric).The data loggers for the Qualimetrics rain gauges have enough memory to record approximately 1500 mm of rainfall. A number of disdrometers will also be deployed as part of the TEFLUN A ground validation program. Three types of disdrometers will be used: 2-D video, Joss, and APL. The 2-D and Joss will be deployed at the profiler site in conjunction with an APL and a tipping bucket rain gauge. The purpose of having all 3 disdrometer types at the profiler types will be to not only compare the surface based measurements of drop size distribution characteristics with the vertical structure (profiler), but also to compare the surface measurements collected by each disdrometer to address the strengths and weaknesses of each unit (address low end sensitivity of the APL disrometer).

    Approximately 5-10 additional APL disdrometers will be used in TEFLUN A. These disdrometers represent a new technology in disdrometer design. They are capable of storing several weeks of data at a time and will be stand-alone units. However, it should be noted that these systems are relatively new (being only deployed in TEFLUN A) and their reliability is not known. Also, as it currently stands, the low-end sensitivity of the APL disdrometer is approximately 1 mm and may therefore bias the retrieved DSD characteristics.


TEFLUN-A Daily Operations *
1 APRIL 1998

During the 1st week of April, no operations took place as the set-up of the project was being completed.

8 APRIL 1998

Forecast: No forecast was available for this day, however, after watching convective events unfold across west Texas, a decision was made to operate the ADRAD. By later in the afternoon, a forecast was made for convection to occur over the gulf on the 9th, which would be ideal for a first ferry flight for the ER-2.

Operations: The ADRAD was operated from 0900 to 1300 UTC on the morning of the 8th to capture a developing squall line out west. The TRMM overpass scheduled at 1200 across the region was not able to capture the mature asymmetric squall line, because the system began to weaken considerably by 1100 UTC.

Side Notes: Field installation of the NASA raingauge network began, and both the NOAA AL Profiler and ETL X-Polimetric radar were operational as well. The TAMU van and truck were being retrofitted with sounding equipment.

9 APRIL 1998

Forecast: No significant chance for convection until 4/12.

Operations: The ER-2 completed the ferry flight over the gulf for calibration purposes. The flight was from Dryden to Eglin AFB landing at 1730 UTC. Useful calibration data over the water was obtained for EDOP and AMPR.

Side Notes: The remaining of 12 raingauges for the surface network was installed along with the 6 APL Disdrometers. Also, the Joss disdromter was placed in close proximity with one of the APL disdrometers at the Profiler site.

10 APRIL 1998

Forecast: No precipitation was expected until the 12th. After which, the long-range forecast was for the chance of convection within the domain for the next few days.

Operations: An alert was scheduled for an ER-2 flight Sunday evening/night (4/12). Special soundings from fellow NWS offices were not requested.

11 APRIL 1998

Forecast: Convection was expected to fire late in the day across north-central Texas with the precipitation area expanding into the region as a front/dryline approached the Texas coast. Precipitation was still forecasted to occur across the domain through the next couple of days.

Operations:The decision was made to cancel the ER-2 flight Sunday night, with possible activation on Monday night (4/13) at 0000 UTC.

Side Notes: All surface based systems were ready for operations as well as the mobile sounding vehicles. One vehicle was sent to HGX while the other stayed at TAMU. All sounding and radar crews were also scheduled.

13 APRIL 1998

Forecast: The cap was still in place across south and central Texas, which would confine the convection off to the north. A convective possibility existed along the front farther east on the 14th, in the Lake Charles region. The extended forecast has area still capped.

Operations: The early alert for operations at 0000 UTC (4/13) was changed for takeoff at 0000 UTC 15 April due to the failed development of convection and the chaotic winds over at Eglin AFB.

Side Notes: The Lear jet was expected to arrive into Texas on the 14th of April.

14 APRIL 1998

Forecast: No organized long-lived precipitation was expected across Texas. Other areas of organized convection would continue along a stationary front in Alabama and Georgia. Parameters were coming together for a convective event over Texas on the 16th.

Operations: There was an ER-2 flight planned for 0000 UTC around central Georgia. X-Pol operated the night before to collect data on drizzle in the Houston area. Another flight was scheduled for Thursday (4/16) as tomorrow was declared a down day due to forecast. The flight over Georgia was a success as all aircraft instruments operated superbly, including the EDOP and AMPR, which collected good data. A calibration check was also performed over the Gulf of Mexico.

15 APRIL 1998

Forecast: Convection continued to fire across north Texas along an old outflow boundary and more was expected to develop along the dryline in central Texas. A slight possibility existed for squall line development and propagation into the area, but there was more confidence in the forecast for convection on Thursday (4/16).

Operations: Declared a down day due to lack of expected precipitation, and for preparations of tomorrow's flight around 1800. The ADRAD was operated to check various calibrations and settings including a check of the antenna controller after a design flaw was corrected.

16 APRIL 1998

Forecast: Uncertainty existed in whether the cap would weaken enough to allow convective development along the front in southeast Texas and Louisiana. Morning soundings taken at CLL and HGX showed the cap stronger than anticipated.

Operations: The scheduled flight was cancelled due to atmospheric trends. Low ceilings and unfavorable winds prevented take-off at Eglin for the ER-2. X-Pol continued to operate since convection was still possible around Houston. A flight was scheduled for the 17th at 0300.

Side Notes: The Lear jet arrived into College Station at 0000 UTC and all systems checked out. The ADRAD's antenna controller problem was fixed and ready to operate.

17 APRIL 1998

Forecast: Widespread convection was expected to develop over the coast along a cold front as an upper level trough swung through the region from old Mexico beginning later in the night and throughout the day Saturday (4/18).

Operations: Alert time was scheduled for the ER-2 flight around 0300, but was later cancelled due to low ceilings at Eglin. Special soundings were launched later in the night at CLL, HGX, CRP, and LCH. A test flight for the Lear was planned for 1830. The ER-2 was put on alert for 1600 UTC tomorrow for the Lake Charles area. The X-Pol operated the entire night and through the day Saturday.

Side Notes: The ADRAD was labeled down until Monday, as some wires and a relay burned up in the antenna controller circuitry. Also, several sounding launches failed at HGX during 2100 to 2330 UTC.

18 APRIL 1998

Forecast: Convection to continue across domain.

Operations: A SW-NE band of weak convection and stratiform rain continued half way between CLL and HOU. NEXRAD showed a strip of 50 dBZ values most of the night. Most of the activity was north of the recently installed raingauge network around Houston early on, but later moved over all of Houston before exiting the area. The TRMM overpass paralleled the activity but was too far south to obtain ideal measurements, although the TMI swath at 1807 was within range. X-Pol operated continuously from 1830 on the 17th to 2030 on the 18th.

The ER-2 flight lasted from 1630 to 2115 UTC with the path over both the profiler and x-pol radar sites. The Lear flight flew from 1753 to 2005 UTC. Other soundings were launched north of the system and within the system from the TAMU van. The aircraft were able to connect for a common flight from the southeast to the northwest along a line at these points. A: 28.42' N 94.15' W to B: 30.26'N 96.00' W. Later, the ER-2 branched off onto another line from C: 29.45'N 95.30 W to D: 29.19'N 93.08' W. Good data was collected by the XPOL, the Profiler, the Lear CPI, EDOP, AMPR, and LIP.

19/20 APRIL 1998

Forecast: No precipitation expected today, but possibility exists for light precip on Monday (4/20).

Operations: None commenced. A plan for a calibration check over the gulf on the 20th with the ER-2 and TRMM satellite was discussed. 21 APRIL 1998

Forecast: Convective and stratiform event will continue north of the area in Texas.

Operations: Initial planned calibration check over the gulf was changed to a coordinated flight with the TRMM overpass north of TAMU. The AMPR contained good data, while the EDOP and LIP failed. The flight consisted of 2 legs across and along the line, which lasted from 0330 to 0915 UTC. Mobile soundings were taken southeast of the band, which was oriented from WSW to ENE across northern Texas.

22/23/24 APRIL 1998

Forecast: No precipitation expected until Sunday (4/26).

Operations: The ER-2 flight was planned for coordination with the TRMM overpass for calibration purposes at 0200 on the 23rd over the east Gulf of Mexico. AMPR collected good data, but the EDOP and LIP failed under clear sky conditions.

25 APRIL 1998

Forecast: Moisture did not return in time to cause convection south of the Red River, therefore nothing was expected in the area. However, better-organized precipitation was possible on Sunday.

Operations: Previous tentative alert for operations was cancelled due to updated forecast. Plans were made for additional soundings at 1700 tomorrow and flight takeoff at 2330 UTC. All other platforms were put on alert for late Sunday.

Side Notes: TAMU truck was delivered back to HGX after improving the antenna reception.

26 APRIL 1998

Forecast: A surface trough forming NW-SE across central Texas was the focus for convective development in the afternoon as instability continued to increase. Widespread deep convection was then progged to move eastward overnight, mainly north of CLL.

Operations: A mobile sounding was taken near Austin at 1700 for forecast purposes, while others were taken during the convective event. FTW special sounding was also taken at 1700.

ER-2 took off at 2330 but aborted the flight early on due to tremendous turbulence from the storms NW of CLL. The EDOP and MAMS instrumentation were accidentally turned off during the first flight line, while strong electrical activity was observed with the LIP. The Lear aborted flight take off due to low ceilings. The ADRAD began collecting data at 2100 UTC. Communication problems were noted between the ADRAD base station and the ER-2.

27 APRIL 1998

Forecast: Elevated convection was noted north of slow moving cold front near CLL-CRP. The area was expected to intensify and continue moving eastward eventually passing through Houston and Louisiana later in the night.

Operations: Previous alert for ER-2 was cancelled due to right roll spoiler failure. ADRAD continued operations from the night before to 0500 4/28. The X-POL took good data as well. Both radars collected data during the 0300 overpass time. The Lear took off at 1610 through 1805 to look at dissipating convection NE of CLL.

Later that night, the jet flew again from 0210 to 0400 UTC to work the TRMM overpass in a convection and stratiform region 60 miles ENE of CLL. Lightning damaged the 2nd transmitter on the plane. CLL and HGX special soundings were taken at 1700, as well as other mobile soundings throughout the event from the TAMU van. Houston took additional soundings at 0000 and 0300 4/28 with additional sonde problems noted.

28 APRIL 1998

Forecast: Nothing significant was expected across the Texas area, but a squall line was progged to form just east of Lake Charles in the afternoon with the front possibly affecting Eglin.

Operations: The ER-2 flight was cancelled and put on standby for 2200 4/29. The Lear took off at 0542 4/29 to target stratiform region near LA coast and to coordinate with TRMM overpass at 0634. X-POL collected data from the Houston area. ADRAD operated from 0000 to 0700. A special sounding was taken by LCH at 0600.

Side Notes: The ER-2 spoiler problem was determined to be an intermittent broken wire. The Lear transmitter was repaired and operational during flight.

29 APRIL 1998

Forecast: Deep convection would continue along stationary front in the Gulf and propagate eastward. Nothing was expected over Texas for awhile.

Operations: Plans were made to alert ER-2 and Lear for a coordinated flight over the Gulf tomorrow night (4/30).

30 APRIL 1998

Forecast: Convection will continue across the southeastern US in the vicinity of Eglin, Alabama, and Georgia. A squall line should develop across N. Alabama and Georgia and move eastward.

Operations: The ER-2 and Lear jet rendezvoused over the southeast from 0000 to 0215 UTC to coordinate with the TRMM overpass at 0057. They flew along the back edge of a mature MCS in the convective and stratiform regions. The ER-2 was able to capture the 0411 overpass as well. During the flight, strong electrical activity was noted as a lightning strike knocked out the new radio and caused an engine problem in the Lear. The ER-2 reported EDOP and LIP failure once again. Strong cells were captured with the AMPR and MIR, while the first MTS data of the project was collected.

1 MAY 1998

Forecast: Only isolated convection was expected across the northeastern Gulf coastal plain, otherwise convective development would occur along a southward moving cold front in Texas by tomorrow afternoon (5/2).

Operations: Plan for a flight tomorrow night. ER-2 alert for takeoff was at 0600 and at 0700 UTC 5/3 for the Lear.

2/3 MAY 1998

Forecast: Front would continue to push offshore and stall in the northern Gulf. Convective activity should continue in the Gulf and in the southeastern US.

Operations: Flight's were cancelled due to lack of the system over Texas not maturing. The ADARD operated from 2100 to 1000 UTC to capture the evolution of the developing storms. TAMU sounding van launched at 0000 and 0500 Saturday evening (5/3). HGX special soundings were also launched Saturday evening.

Side Notes: The MAMS instruments were replaced by the SLS on the ER-2.

4 MAY 1998

Forecast: With a front stalled across the southern area near Houston, convective development was possible over the region along the front. Also, more convection was expected over the southeast near Eglin.

Operations: Good coordination was obtained with the TRMM overpass at 2146. EDOP, AMPR, LIP, and MIR all collected good data. Strong electrical activity was observed with the squall line and most of the stratiform region was over Southern Florida.

6 MAY 1998

Forecast: The cap would continue for Texas while convection fired over from Kansas to Arkansas. Other convection would continue in the Midwest and in the southeastern US.

Operations: A joint flight was attempted with the Lear and ER-2 over Florida at 1820 UTC for a convective system along the MS/AL coastline. Communication was disrupted between the two causing a missed event for the ER-2, which returned to Dryden AFB. The Lear jet flew an additional flight over the same area near Mobile from 2135 to 2247 to gather more cloud physics data before refueling and returning to CLL. 8 MAY 1998

Forecast: Supercellular convection was expected across NW Texas along a warm front/dryline interaction by afternoon. With time, cells were expected to evolve into a squall line system and propagate eastward.

Operations: The TAMU sounding van launched several sondes in NW Texas. The ADRAD began collecting data from 0300 to 0900 UTC (5/9). The Lear jet penetrated a supercell anvil at 2351 to 0111 before aborting the mission.

Data Availability & Summary: TEFLUN Data Protocol list
marker TEFLUN Data Category list
marker TEFLUN Priority Days list
marker Data Availability Schedule list
marker Tables of Flight Logs & Measurements list
marker Coincidences of Ground, Aircraft & Satellite Measurements list
marker TEFLUN-A Flight Scenarios list
marker Field Measurement Locations list
marker Soundings Report


Data Access:

TEFLUN data resides on DISC anonymous FTP. You may access the files from this document, FTP
GIFTEFLUN Data

or directly via FTP at ftp disc2.nascom.nasa.gov
login: anonymous
password: < your internet address >
cd data/TEFLUNA/


Last update:Mon Jan 5 08:54:43 EST 2004
>

Page Author: Hydrology Data Support Team -- hydrology-disc@listserv.gsfc.nasa.gov
Web Curator: -- Website Curator: Anthony Drake
NASA official: Steve Kempler, DISC Manager -- kempler@disc.gsfc.nasa.gov
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