MESO-SAILS

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SAILS concept. NEXRAD MESO-SAILS scanning strategy.png
SAILS concept.

Multiple Elevation Scan Option for Supplemental Adaptive Intra-Volume Low-Level Scan [1] (abbreviated MESO-SAILS), [2] is a dynamic scanning option for the WSR-88D, controllable by the operator of the radar, when in VCP mode 12 and 212, and additionally 35 and 215 with the Build 18 update scheduled for October 2017. When active, anywhere from one to three supplemental low-level scans can be added to any volume, increasing overall low-level data availability and improves general severe weather detection, as needed. When active, per the National Weather Service, low-level updates will be available "every 75 to 90 seconds". [3]

Contents

Concept

WSR-88D radars scan a number of elevation angles to scan the atmosphere around the site. The number of angles and the length of each scan depend on the meteorological situation (no precipitation, scattered, generalized, or deep convective precipitation). These schemes are called Volume Coverage Patterns (VCP). [2]

The more angles scanned, the longer between scans at the lowest elevation. Data at that level can be crucial in summer thunderstorm situations when Doppler patterns for rotations and windshifts, as well as dual polarized information, are indicative of severe weather like tornadoes. Shortening the time between two scans at low level is therefore an important factor for convective storm detection. The first step of this program is SAILS (Supplemental Adaptive Intra-Volume Low-Level Scan) which inserts an extra scan of the elevation defined in the VCP definition (normally 0.5°). [2] This is done by forcing the antenna to go back down to the base elevation after scanning a certain number elevations up to the "middle" of the atmosphere, this "middle" elevation being dependent of the VCP used. [2] Doing this provides two low-level scans for each total volume scan while only adding 30 to 35 seconds to the total scan. [2]

To increase the number of low-level scans, one can redo the same process as SAILS many times: MESO-SAILS (Multiple Elevation Scan Option for SAILS). These additional supplemental low-level elevation scans are evenly spaced, in time (as close as possible given the defined VCP rotation rates), throughout the volume scan. [2] The radar operator may choose 1 to 3 extra scans, depending on the weather situation. This lengthens the time of the total scan but provide low-level coverage more often. [2]

History and deployment

During the summer of 2013, the Radar Operations Center, in order to facilitate "proof of concept" testing of MESO-SAILS, defined two VCPs that were based on VCP-12 that included hardcoded additional low-level split-cut scans. [2] For the first testing, which commenced on June 26, 2013, SAILSx2 (2 supplemental low-level soundings) was executed for approximately 4+12 hours, and during the testing a radar technician observed the behavior of the pedestal/antenna assembly. No excessive wear was noted to the assembly of the KOUN radar in Norman, Oklahoma.

Two days later, June 28, 2013, SAILSx3 (3 supplemental low-level soundings) was executed, also within the KOUN RPG. During this 1+12-hour test of SAILSx3, a ROC radar hardware engineer accompanied the ROC electronics maintenance technician to observe the antenna/pedestal assembly. Again, no excessive wear was noted. [4]

MESO-SAILS was thus deployed with Build 14 update in the spring of 2014 and is still in operations when needed. [5] The operator can choose between 1, 2, or 3 supplemental low-level scans with MESO-SAILS active.

MESO-SAILS in tornado cases

A study published in 2016 looked at how the MESO-SAILS radar scanning regime performed with respect to tornado debris signature (TDS) detection during the 2016 tornado season in the Iowa Region, compared to the distribution before its implementation. When tornado watches were active, MESO-SAILS was active 100% reflecting the National Weather Service expectations for such situations. Overall, it was found that the use of MESO-SAILS led to an enhancement in detection and possibly an increased effective range at which TDSs could be detected. [6] The use of MESO-SAILS dropped to 41% during severe thunderstorms watches however, which may suggest some benefit in keeping MESO-SAILS active during severe thunderstorm watches as well. [6]

Related Research Articles

Mesocyclone Region of rotation within a powerful thunderstorm

A mesocyclone is a meso-gamma mesoscale region of rotation (vortex), typically around 2 to 6 mi in diameter, most often noticed on radar within thunderstorms. In the northern hemisphere it is usually located in the right rear flank of a supercell, or often on the eastern, or leading, flank of a high-precipitation variety of supercell. The area overlaid by a mesocyclone’s circulation may be several miles (kn) wide, but substantially larger than any tornado that may develop within it, and it is within mesocyclones where intense tornadoes form.

Tornado warning Weather warning indicating imminent danger of tornadoes

A tornado warning is a severe weather warning product issued by regional offices of weather forecasting agencies throughout the world to alert the public when a tornado has been reported or indicated by weather radar within the parent severe thunderstorm. It can be issued after a tornado, funnel cloud and rotation in the clouds has been witnessed by the public, storm chasers, emergency management or law enforcement, and indicates that residents in the affected areas should take immediate safety precautions.

Tornado watch Weather watch indicating conditions favorable for tornado development in severe thunderstorms

A tornado watch is a severe weather watch product issued by national weather forecasting agencies when meteorological conditions are favorable for the development of severe thunderstorms capable of producing tornadoes. In addition to the potential for tornado development, thunderstorms that develop within the watch area may contain large hail, straight-line winds, intense rainfall and/or flooding that pose a similar damage risk as the attendant tornado threat. A watch must not be confused with a tornado warning.

National Weather Service U.S. forecasting agency of the National Oceanic and Atmospheric Administration

The National Weather Service (NWS) is an agency of the United States federal government that is tasked with providing weather forecasts, warnings of hazardous weather, and other weather-related products to organizations and the public for the purposes of protection, safety, and general information. It is a part of the National Oceanic and Atmospheric Administration (NOAA) branch of the Department of Commerce, and is headquartered in Silver Spring, Maryland, within the Washington metropolitan area. The agency was known as the United States Weather Bureau from 1890 until it adopted its current name in 1970.

NEXRAD Nationwide network of Doppler weather radars operated by the U.S. National Weather Service

NEXRAD or Nexrad is a network of 160 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.

Weather radar 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.

Hook echo Weather radar signature indicating tornadic circulation in a supercell thunderstorm

A hook echo is a pendant or hook-shaped weather radar signature as part of some supercell thunderstorms. It is found in the lower portions of a storm as air and precipitation flow into a mesocyclone, resulting in a curved feature of reflectivity. The echo is produced by rain, hail, or even debris being wrapped around the supercell. It is one of the classic hallmarks of tornado-producing supercells. The National Weather Service may consider the presence of a hook echo coinciding with a tornado vortex signature as sufficient to justify issuing a tornado warning.

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).

Anticyclonic tornado Tornado that spins clockwise

An anticyclonic tornado is a tornado which rotates in a clockwise direction in the Northern Hemisphere and a counterclockwise direction in the Southern Hemisphere. The term is a naming convention denoting the anomaly from normal rotation which is cyclonic in upwards of 98 percent of tornadoes. Many anticyclonic tornadoes are smaller and weaker than cyclonic tornadoes, forming from a different process, as either companion/satellite tornadoes or nonmesocyclonic tornadoes.

Bounded weak echo region Weather feature

The bounded weak echo region, also known as a BWER or a vault, is a radar signature within a thunderstorm characterized by a local minimum in radar reflectivity at low levels which extends upward into, and is surrounded by, higher reflectivities aloft. This feature is associated with a strong updraft and is almost always found in the inflow region of a thunderstorm. It cannot be seen visually. The BWER has been noted on radar imagery of severe thunderstorms since 1973 and has a lightning detection system equivalent known as a lightning hole.

Volumetric Imaging and Processing of Integrated Radar, known by the acronym VIPIR, is an analysis and display program for Doppler weather radar, created and sold by Baron Services. This software allows improved analysis of radar data for private users, in particular television stations, similar to the Weather Decision Support System program used by the National Weather Service.

Tornadogenesis Process by which a tornado forms

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WSR-1

The WSR-1 or Weather Surveillance Radar-1 was one of the first weather radars and the first used by a civilian organization in the US. The WSR-1 series was a modified version of the AN/APS-2F radar, which the Weather Bureau acquired from the Navy. The WSR-1A, WSR-3, and WSR-4 were also variants of this radar. The first WSR-1 in the USA was at Washington National Airport in Washington, D.C. in 1947, and the last WSR-3 was retired by 1978.

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.

Tornado vortex signature

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, but it is not an important feature in the National Weather Service's warning operations.

Hail spike Weather radar indicator of hail

A hail spike or three body scatter spike (TBSS) is an artifact on a weather radar display indicative of large hail. They are identified by a spike of weak reflectivity echoes that extend out from a thunderstorm, and away from the radar site.

Terminal Doppler Weather Radar

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. 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.

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

National Weather Service Kansas City/Pleasant Hill, Missouri

National Weather Service - Pleasant Hill/Kansas City, Missouri is a Weather Forecast Office (WFO) of the National Weather Service, which is responsible for forecasts and the dissemination of weather warnings and advisories for 37 counties in northern and western Missouri and seven counties in extreme eastern Kansas, including the Kansas City and St. Joseph metropolitan areas. Though, as the Storm Prediction Center (SPC) in Norman, Oklahoma is responsible for issuing severe thunderstorm and tornado watches, the Pleasant Hill/Kansas City WFO only composes outline and status updates for SPC-issued watches affecting any portion of its designated County Warning Area.

Tornado outbreak of November 30 – December 2, 2018 Weather event in the central US

The tornado outbreak of November 30 – December 2, 2018 was a late-season tornado outbreak that occurred across portions of the West South Central states and Midwestern United States. As a potent shortwave trough moved across the southern portions of the country, it was met with ample moisture return and destabilization, resulting in widespread severe thunderstorms that produced damaging winds, hail, and tornadoes. The event began late on November 30 in Oklahoma, spreading east and resulting in one fatality in Aurora, Missouri. Several tornadic supercells moved across portions of Illinois on December 1, and resulted in 29 confirmed tornadoes. This outbreak was the largest December tornado event on record in Illinois history, surpassing the December 1957 tornado outbreak sequence. The most significant tornado of the event was an EF3 that impacted Taylorville, Illinois, damaging or destroying hundreds of structures and injuring 22 people.

References

  1. WDT Support (July 7, 2015). "What is SAILS mode". Radarscope. Archived from the original on February 4, 2017. Retrieved February 3, 2017.
  2. 1 2 3 4 5 6 7 8 Radar Operations Center (ROC (February 2014). "MESO-SAILS (Multiple Elevation Scan Option for SAILS): Initial Description Document" (PDF).
  3. "MES0-SAILS Test: New Radar Technology". www.weather.gov.
  4. "MESO-SAILS Test Report" (PDF). ROC Web Page. July 2013.
  5. wdssiidevelopers (April 22, 2015). "SAILING". Wordpress.
  6. 1 2 Miller, Cameron J. A. (December 2016). A Preliminary Evaluation of MESO-SAILS Tornadic Debris Signature Detection and its Use in the Iowa Region (Senior thesis). Iowa State University. doi: 10.31274/mteor_stheses-180813-10 .

Bibliography