RaXPol

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RaXPol (Rapid X-band Polarimetric Radar)
RaXPol scanning a severe thunderstorm in Oklahoma May 18, 2013.JPG
RaXPol scanning a severe thunderstorm in Oklahoma
Country of originUSA
Introduced2011
No. built1
TypeWeather radar
Frequency9.73 GHz (X Band)
PRF Adjustable 1,000 to 8,000 Hz
Beamwidth 1.0°
PulsewidthAdjustable 0.1 to 40 μs
RPMup to 30 rpm
Diameter2.4 m (7.9 ft)
Azimuth 360°
Power20 kW

The RapidX-bandPolarimetric Radar, commonly abbreviated as RaXPol, [1] is a mobile research radar designed and operated by the University of Oklahoma, led by Howard Bluestein. RaXPol often collaborates with adjacent mobile radar projects, such as Doppler on Wheels and SMART-R. [2] Unlike its counterparts, RaXPol typically places emphasis on temporal resolution, and as such is capable of surveilling the entire local atmosphere in three dimensions in as little as 20 seconds, or a single level in less than 3 seconds. [3]

Contents

History and deployment

Ever since meteorological observations on radar were first made widespread, the need for high-temporal resolution and comprehensive volumetric imagery of all three dimensions of weather phenomena has been a very high priority, due in large part to the fact that hazardous weather often happens in the span of seconds, and often in the lowest 1 kilometer of the atmosphere. [4] In pursuit of better resolution in time, the NEXRAD network deploys several time-saving measures to accelerate data rates in these three dimensions, such as M.R.L.E. and MESO-SAILS, which can be bringing scan time down from 5–7 minutes to 2–3 minutes. In 2010, the University of Oklahoma's Advanced Radar Research Center began development of RaXPol, with a focus on rapid deployment and analysis of the atmosphere. [1] By early 2011, RaXPol was being deployed in field campaigns across Tornado Alley, and has taken part in numerous NSF funded research projects and organizations, such as PECAN, [5] TORUS, [6] and IMPACTS. [7]

Findings

RaXPol has documented numerous hazardous weather events throughout its deployment history, among them being several dozen particularly intense tornadoes. On May 24, 2011, RaXPol observed an extremely violent EF-5 tornado near El Reno, Oklahoma at very high temporal resolution, measuring doppler velocities in excess of 250 mph. [8] Two years later, RaXPol observed the widest tornado in recorded history (2.6 miles wide), also near the town of El Reno, retrieving among the highest doppler velocities ever recorded at 295 mph. Based on this data, the tornado was initially rated EF-5, but was later downgraded to an EF-3 due to the lack of supporting damage on the ground. [9] Data gathered from RaXPol also indicates that the formation of tornadoes may not be a top-down process as was once thought. [10]

Related Research Articles

<span class="mw-page-title-main">Tornado</span> Violently rotating column of air in contact with both the Earths surface and a cumulonimbus cloud

A tornado is a violently rotating column of air that is in contact with both the surface of the Earth and a cumulonimbus cloud or, in rare cases, the base of a cumulus cloud. It is often referred to as a twister, whirlwind or cyclone, although the word cyclone is used in meteorology to name a weather system with a low-pressure area in the center around which, from an observer looking down toward the surface of the Earth, winds blow counterclockwise in the Northern Hemisphere and clockwise in the Southern. Tornadoes come in many shapes and sizes, and they are often visible in the form of a condensation funnel originating from the base of a cumulonimbus cloud, with a cloud of rotating debris and dust beneath it. Most tornadoes have wind speeds less than 180 kilometers per hour, are about 80 meters across, and travel several kilometers before dissipating. The most extreme tornadoes can attain wind speeds of more than 480 kilometers per hour (300 mph), are more than 3 kilometers (2 mi) in diameter, and stay on the ground for more than 100 km (62 mi).

<span class="mw-page-title-main">NEXRAD</span> Network of weather radars operated by the NWS

NEXRAD or Nexrad is a network of 159 high-resolution S-band Doppler weather radars operated by the National Weather Service (NWS), an agency of the National Oceanic and Atmospheric Administration (NOAA) within the United States Department of Commerce, the Federal Aviation Administration (FAA) within the Department of Transportation, and the U.S. Air Force within the Department of Defense. Its technical name is WSR-88D.

<span class="mw-page-title-main">Tornado records</span> List of world records related to tornadoes

This article lists various tornado records. The most "extreme" tornado in recorded history was the Tri-State tornado, which spread through parts of Missouri, Illinois, and Indiana on March 18, 1925. It is considered an F5 on the Fujita Scale, even though tornadoes were not ranked on any scale at the time. It holds records for longest path length at 219 miles (352 km), longest duration at about 3½ hours, and it held the fastest forward speed for a significant tornado at 73 mph (117 km/h) anywhere on Earth until 2021. In addition, it is the deadliest single tornado in United States history with 695 fatalities. It was also the third most costly tornado in history at the time, but has been surpassed by several others non-normalized. When costs are normalized for wealth and inflation, it still ranks third today.

<span class="mw-page-title-main">Weather radar</span> Radar used to locate and monitor meteorological conditions

Weather radar, also called weather surveillance radar (WSR) and Doppler weather radar, is a type of radar used to locate precipitation, calculate its motion, and estimate its type. Modern weather radars are mostly pulse-Doppler radars, capable of detecting the motion of rain droplets in addition to the intensity of the precipitation. Both types of data can be analyzed to determine the structure of storms and their potential to cause severe weather.

<span class="mw-page-title-main">Multiple-vortex tornado</span> Tornado comprising multiple vortices

A multiple-vortex tornado is a tornado that contains several vortices revolving around, inside of, and as part of the main vortex. The only times multiple vortices may be visible are when the tornado is first forming or when condensation and debris are balanced such that subvortices are apparent without being obscured. They can add over 100 mph to the ground-relative wind in a tornado circulation and are responsible for most cases where narrow arcs of extreme destruction lie right next to weak damage within tornado paths.

The National Severe Storms Laboratory (NSSL) is a National Oceanic and Atmospheric Administration (NOAA) weather research laboratory under the Office of Oceanic and Atmospheric Research. It is one of seven NOAA Research Laboratories (RLs).

<span class="mw-page-title-main">Doppler on Wheels</span> Fleet of X-band radar trucks maintained by the Center for Severe Weather Research (CSWR)

Doppler on Wheels is a fleet of X-band and C-band radar trucks managed by the University of Illinois Urbana-Champaign and previously maintained by the Center for Severe Weather Research (CSWR) in Boulder, Colorado, led by principal investigator (PI) Joshua Wurman, with the funding largely provided by the National Science Foundation (NSF). The DOW fleet and its associated Mobile Mesonets and deployable weather stations (Pods) were Lower Atmospheric Observing Facilities (LAOF) "National Facilities" supporting a wide variety NSF-sponsored research. They are now included in the NSF's "Community Instruments and Facilities" (CIF) program led by PI Karen Kosiba.

Convective storm detection is the meteorological observation, and short-term prediction, of deep moist convection (DMC). DMC describes atmospheric conditions producing single or clusters of large vertical extension clouds ranging from cumulus congestus to cumulonimbus, the latter producing thunderstorms associated with lightning and thunder. Those two types of clouds can produce severe weather at the surface and aloft.

<span class="mw-page-title-main">Joshua Wurman</span> American meteorologist

Joshua Michael Aaron Ryder Wurman is an American atmospheric scientist and inventor noted for tornado, tropical cyclone, and weather radar research.

<span class="mw-page-title-main">Tornado vortex signature</span>

A tornadic vortex signature, abbreviated TVS, is a Pulse-Doppler radar weather radar detected rotation algorithm that indicates the likely presence of a strong mesocyclone that is in some stage of tornadogenesis. It may give meteorologists the ability to pinpoint and track the location of tornadic rotation within a larger storm, and is one component of the National Weather Service's warning operations.

<span class="mw-page-title-main">VORTEX projects</span>

The Verification of the Origins of Rotation in Tornadoes Experiment are field experiments that study tornadoes. VORTEX1 was the first time scientists completely researched the entire evolution of a tornado with an array of instrumentation, enabling a greater understanding of the processes involved with tornadogenesis. A violent tornado near Union City, Oklahoma was documented in its entirety by chasers of the Tornado Intercept Project (TIP) in 1973. Their visual observations led to advancement in understanding of tornado structure and life cycles.

<span class="mw-page-title-main">OU-PRIME</span>

OU-PRIME was an advanced Doppler weather radar. It was completed in January 2009 after a ten-month construction period and commissioned on April 4, 2009. It is operated by the Advanced Radar Research Center (ARRC) at the University of Oklahoma (OU). The radar was manufactured by Enterprise Electronics Corporation to provide OU students and faculty a platform for research and education in the field of radar meteorology. This C-band polarimetric radar has some of the highest resolution data of any C-band weather radar in the United States.

<span class="mw-page-title-main">Terminal Doppler Weather Radar</span>

Terminal Doppler Weather Radar (TDWR) is a Doppler weather radar system with a three-dimensional "pencil beam" used primarily for the detection of hazardous wind shear conditions, precipitation, and winds aloft on and near major airports situated in climates with great exposure to thunderstorms in the United States. As of 2011, all were in-service with 45 operational radars, some covering multiple airports in major metropolitan locations, across the United States & Puerto Rico. Several similar weather radars have also been sold to other countries such as China (Hong Kong). Funded by the United States Federal Aviation Administration (FAA), TDWR technology was developed in the early 1990s at Lincoln Laboratory, part of the Massachusetts Institute of Technology, to assist air traffic controllers by providing real-time wind shear detection and high-resolution precipitation data.

<span class="mw-page-title-main">Tornado outbreak sequence of May 21–26, 2011</span> United States meteorological event

From May 21 to May 26, 2011, one of the largest tornado outbreaks on record affected the Midwestern and Southern regions of the United States. A six-day tornado outbreak sequence, most of the tornadoes developed in a corridor from Lake Superior southwest to central Texas, while isolated tornadoes occurred in other areas. An especially destructive EF5 tornado destroyed one-third of Joplin, Missouri, resulting in 158 deaths and over 1,000 injuries. The Joplin tornado was the deadliest in the United States since April 9, 1947, when an intense tornado killed 181 in the Woodward, Oklahoma, area. Tornado-related deaths also occurred in Arkansas, Kansas, Minnesota, and Oklahoma. Overall, the tornado outbreak resulted in 186 deaths, 8 of those non-tornadic, making it second only to the 2011 Super Outbreak as the deadliest since 1974. It was the second costliest tornado outbreak in United States history behind that same April 2011 outbreak, with insured damage estimated at $4–7 billion.

<span class="mw-page-title-main">2013 El Reno tornado</span> Widest and second-strongest tornado ever recorded

During the early evening of Friday, May 31, 2013, an extremely large and powerful tornado occurred over rural areas of Central Oklahoma. This rain-wrapped, multiple-vortex tornado was the widest tornado ever recorded and was part of a larger weather system that produced dozens of tornadoes over the preceding days. The tornado initially touched down at 6:03 p.m. Central Daylight Time (2303 UTC) about 8.3 miles (13.4 km) west-southwest of El Reno, rapidly growing in size and becoming more violent as it tracked through central portions of Canadian County. Remaining over mostly open terrain, the tornado did not impact many structures; however, measurements from mobile weather radars revealed extreme winds up to 135.0 m/s within the vortex. These are among the highest observed wind speeds on Earth, just slightly lower than the wind speeds of the 1999 Bridge Creek–Moore tornado. As it crossed U.S. 81, it had grown to a record-breaking width of 2.6 miles (4.2 km), beating the previous width record set in 2004. Turning northeastward, the tornado soon weakened. Upon crossing Interstate 40, the tornado dissipated around 6:43 p.m. CDT (2343 UTC), after tracking for 16.2 miles (26.1 km), it avoided affecting the more densely populated areas near and within the Oklahoma City metropolitan area.

The following is a glossary of tornado terms. It includes scientific as well as selected informal terminology.

<span class="mw-page-title-main">Multifunction Phased Array Radar</span>

Multifunction Phased Array Radar (MPAR) was an experimental Doppler radar system that utilized phased array technology. MPAR could scan at angles as high as 60 degrees in elevation, and simultaneously track meteorological phenomena, biological flyers, non-cooperative aircraft, and air traffic. From 2003 through 2016, there was one operational MPAR within the mainland United States—a repurposed AN/SPY-1A radar set loaned to NOAA by the U.S. Navy. The MPAR was decommissioned and removed in 2016.

<span class="mw-page-title-main">Tennessee Valley Weather</span> Television station in Alabama, United States

Tennessee Valley Weather is a television station owned by Tennessee Valley Media Group, headquartered in Lawrenceburg, Tennessee. It services North Alabama, Southern Tennessee, and Northeast Mississippi with daily weather updates and local severe weather information. The combined network broadcasts over-the-air updates, social media posts, and produces live content on a digital streaming television channel available on a host of Internet based platforms, as well as local cable providers.

<span class="mw-page-title-main">2011 El Reno–Piedmont tornado</span> 2011 EF-5 tornado in the U.S. state of Oklahoma

<span class="mw-page-title-main">Advanced Technology Demonstrator</span>

Advanced Technology Demonstrator (ATD) is an experimental weather radar system using Phased Array technology seeking to enhance Phased Array capabilities with the addition of dual-polarity and pulse compression. It's predecessor, MPAR, was the first large-scale PAR experiment taken on by NOAA in 2003, and was deployed until it's eventual decommission in favor of ATD in 2016.

References

  1. 1 2 "A Mobile Rapid-Scanning X-band Polarimetric (RaXPol) Doppler Radar System in: Journal of Atmospheric and Oceanic Technology Volume 30 Issue 7 (2013)". journals.ametsoc.org. Retrieved 2022-10-24.
  2. "PECAN Fixed & Mobile Radars | Earth Observing Laboratory". eol.ucar.edu. Retrieved 2022-10-24.
  3. "Advanced Radar Research Center". arrc.ou.edu. Retrieved 2022-10-24.
  4. "Faster Radar Data Means More Advanced Warning for Hazardous Weather". weather.gov. Retrieved 2022-10-24.
  5. "PECAN | Earth Observing Laboratory". eol.ucar.edu. Retrieved 2022-10-24.
  6. "NSSL Projects:TORUS: Targeted Observations by Radars and UAS of Supercells". nssl.noaa.gov. Retrieved 2022-10-24.
  7. "OU researchers team up with NASA to study January nor'easter | StateImpact Oklahoma". stateimpact.npr.org. Retrieved 2022-10-24.
  8. "Observations of Supercell Tornado Evolution Using a Mobile, Rapid-Scan, X-Band Radar". shareok.org. Retrieved 2022-10-24.
  9. "El Reno, Oklahoma tornado downgraded to EF-3 | Earth". EarthSky. Retrieved 2022-10-24.
  10. "Abstract: Confirming Bottom-up Tornadogenesis in the 31 May 2013 El Reno Tornado (29th Conference on Severe Local Storms)". ams.confex.com. Retrieved 2022-10-24.