WSR-1

Last updated
WSR-1 – 4 [1]
WSR-1 radar and radiosonde dome North Omaha Airport.jpg
The upper air and radar (WSR-1) site, on the left, at the North Omaha Airport from 1954 to 1974.
Country of originUnited States
Introduced1946
No. built82
Type Weather radar
Frequency3.3 GHz (S band)
PRF 325 and 650 Hz
Beamwidth 3.5°
Pulsewidth1 and 2μs excepted 1 and 4 μs on WSR-4
Rangemore than 100 kilometres (62 mi)
Diameter2 m
Azimuth 0 to 360º
Elevation-2 to 50º
Power50 kW

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. [2] The WSR-1 series was a modified version of the AN/APS-2F radar, which the Weather Bureau (now the National Weather Service) acquired from the Navy. The WSR-1A, WSR-3, and WSR-4 were also variants of this radar. [1] The first WSR-1 in the USA was at Washington National Airport in Washington, D.C., in 1947, [1] and the last WSR-3 was retired by 1978. [3]

Contents

History

In 1946, the US Weather Bureau (ancestor of the National Weather Service) retrieved 25 AN/APS-2F aeronautical radars from the US Navy. The radars have been modified and adapted to meteorology and then delivered at the rate of five per year. The modifications were conducted by the weather service and the modified radars took the successive names of WSR-1, WSR-1A, WSR-3 and WSR-4, depending on the gradual improvement of hardware. [1] The first WSR-1 was put into service at the Washington, DC, national airport on March 12, 1947. The second began service on June 1, 1947 in Wichita, Kansas, in the heart of the Tornado Alley. [1] In August of the same year, the WSR-1 installed at Norfolk, Nebraska proved its usefulness and cost savings by alerting the Elkhorn Valley power system of the approach of thunderstorms. [1]

Three particularly severe weather events occurred during the spring of 1953 and led to the establishment of the Texas Tornado Warning Network. Major cities in Texas have been asked to fund the operation (both the private and public sectors) of modifying and implementing the WSR-1, WSR-1A, WSR-3 and WSR-4. The Weather Bureau agreed to operate these radars and maintain them in order to alert the public in case of danger, as soon as a visual confirmation was obtained. The establishment of the network became effective during a kick-off meeting on June 24, 1953. [1] It took nearly six years for the network to be fully operational; 17 radars have been modified and installed thanks to the joint efforts of local authorities, the state, federal agencies and a university. [1]

The APS-2F modified by Texas A & M University, although not actually part of the tornado surveillance network, was at least once used for warning purposes on April 5, 1956. [1] After 1956 the modification of the APS-2F radars in their WSR-1, WSR-1A, WSR-3 and WSR-4 versions was assigned to the Weather Office headquarters which had to move some antennas that had originally been installed to locations where it was difficult to ensure the maintenance. [1]

In April 1975, at the peak of the program, 82 WSR-1, WSR-1A, WSR-3 and WSR-4 were in service. [1] Some were replaced by WSR-57s, but most remained in service until they were replaced by WSR-74s during a period from 1976 to 1980. [1] No more remains in service today.

Characteristics

Meriden, Kansas, tornado as observed by the Topeka Weather Bureau WSR-3 radar. Meriden, Kansas, tornado as observed by the Topeka Weather Bureau WSR-3 radar.jpg
Meriden, Kansas, tornado as observed by the Topeka Weather Bureau WSR-3 radar.

The WSR-1 to 4 series, the first operational weather radar in the United States, used the AN/APS-2F electronics, including a superheterodyne receiver, but with a larger antenna. As time progressed and experience with the original design increased, the Weather Bureau felt confident enough to upgrade the WSR-1 to WSR-1A, eventually finalizing on the WSR-3 and WSR-4 model. The WSR-4 upgrades included the removal of the original aircraft-oriented antenna in favor of a larger antenna, and the addition of a power converter such that it would now have the ability to function on conventional power. [1]

The main difference between the versions was their display and the control of the probed atmospheric volume. The diameter of the dish was nearly 2 meters by the WSR-4. The wavelength used was about 10 cm which corresponds to a frequency of 3 GHz. This frequency is in the S band which is still used by the current US weather radar network. Thanks to the radars operative frequency, the attenuation due to the rain was almost zero, [4] but the detection of a light rain or snow was delicate because of the weakness of the signal emitted by the radar (50 kW). [1]

WSR-3 console WSR-57 Weather Radar Console.jpg
WSR-3 console

The WSR-1 used a panoramic display (PPI) placing weather echoes in azimuth/distance coordinates on a circular screen whose center represented the position of the radar, and also a linear oscilloscope (A-Scope) showing the intensity of the echoes according to their distance from the radar. [1] Everything was mounted on a rack. The WSR-3 and WSR-4 used A-Scope displays and height/distance displays (RHI) which allows a vertical sectional view in a chosen direction. They were mounted next to each other on a console. The WSR-1A used the same displays but stacked vertically. From a technical point of view, the WSR-4 had a traveling-wave tube that improved the sensitivity compared to the WSR-3. [1]

Radar Sites

NWS office and WSR-3 radar Hunstville International Airport NWS office and WSR-3 radar Hunstville International Airport.jpg
NWS office and WSR-3 radar Hunstville International Airport

The 82 radar sites of WSR1, 1A, 3 and 4 are listed below

WSR-1 and 1A sites [3]
LocationCommissionedDecommissionedReplaced by
Baton Rouge, LAAugust 16, 19551973?
Burrwood, LA19561960WSR-4
Fort Worth, TXApril 21, 1954April 1961WSR-57
Hartford, CT19551959WSR-3
Dodge City, KSJune 13, 1954July 25, 1963WSR-3
Lubbock, TX1954August 1972WSR-74C
Norfolk, NEJuly 27, 19471976WSR-74C
North Omaha, NE19551977WSR-74C
Oklahoma City, OKMarch 1, 19551960WSR-57
Philadelphia, PANovember 20, 1959 ?
Pittsburgh, PA1952?October 4, 1963
Port Arthur, TXJuly 15, 1955 ?
St. Louis, MOJune 19551960WSR-57
Shreveport, LANovember 19551976WSR-74C
Sioux Falls, SD19561976?WSR-74C
Springfield, MOJune 28, 1957 ?
Tampa, FL19561960WSR-57
Topeka, KS19531957WSR-3
Tulsa, OKMay 4, 19561976WSR-74C
Waco, TXApril 28, 19551976WSR-74C
Washington, DCMarch 12, 1947 ?
Wichita, KSJune 1, 1947June 5, 1956WSR-3
Wichita Falls, TXApril 25, 1956
(Replaced a military APS-2F radar)
1977WSR-74C
Worcester, MAMarch 16, 19561976WSR-74C
WSR-3 sites [3]
LocationCommissionedDecommissionedReplaced by
Abilene, TX25 March 197227 August 1977WSR-74C
Albany, NY12 November 195827 July 1977WSR-74C
Astoria, OR1 June 19591 November 1967
Binghamton, NY15 June 19598 March 1978WSR-74S
Chicago/Midway, IL19 April 1958January 1963WSR-57
Cleveland, OH13 May 1957WSR-74C
Columbia, MOAugust 1957November 1977WSR-74C
Columbus, OH12 February 195919 January 1977
Détroit, MI1 May 195712 September 1962WSR-57
Dodge City, KS25 July 196325 July 1972
Eureka, CA1957June 1972Given to California State University in Humboldt
Flint, MI15 November 195715 January 1978
Fort Smith, AR30 August 196029 December 1975WSR-74C
Fort Wayne, IN195712 March 1976WSR-74C
Hartford, CT29 April 1959April 1977WSR-74C
Hunstville, ALOctober 19581977WSR-74C
LocationCommissionedDecommissionedReplaced by
Indianapolis, INOctober 1959September 1977WSR-74C
Jackson, MS19591969WSR-57
Little Rock, AR19 December en remplacement d'un AN/APS-2E militaire19 April 1962WSR-57
Macon, GA21 April 195818 April 1977WSR-74C
Madison, WI29 March 195815 May 1979WSR-74C
Memphis, TN1957 ?
Meridian, MS16 August 19592 November 1976WSR-74C
Miami, FLDurant la Seconde Guerre mondiale ?
Montgomery, ALOctober 19581971WSR-74C in 1977
Muskegon, MI9 May 195725 March 1976WSR-74C
Nashville, TN2 April 195731 October 1970WSR-57
Richmond, VA7 July 1958October 1959
Rochester, MNSeptember 1960April 1976WSR-74C
Scottbluff, MOSummer 19691978
Tatoosh Island, WA1 October 1960January 1964
Topeka, KS19571976WSR-74C
Wichita, Kansas 5 June 195622 June 1960WSR-57
WSR-4 sites [3]
LocationCommissionedDecommissionedReplaced by
Burrwood, LA1960 ?
Concordia, KS1 June 196218 February 1977WSR-74C
Savannah, GA7 April 19601970

Related Research Articles

<span class="mw-page-title-main">National Weather Service</span> 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.

<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">WSR-74</span> Weather surveillance radar

WSR-74 radars were Weather Surveillance Radars designed in 1974 for the National Weather Service. They were added to the existing network of the WSR-57 model to improve forecasts and severe weather warnings. Some have been sold to other countries like Australia, Greece, and Pakistan.

<span class="mw-page-title-main">WSR-57</span> Weather radar used by the U.S. Weather Bureau

WSR-57 radars were the primary weather surveillance radar used by the United States for over 35 years. The National Weather Service operated a network of this model radar across the country, watching for severe weather.

<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">Hook echo</span> 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 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).

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

The Aggie Doppler Radar (ADRAD) is a Doppler weather radar located on the roof of the Eller Oceanography & Meteorology Building on the Texas A&M University campus in College Station, Texas.

<span class="mw-page-title-main">Canadian weather radar network</span> Weather radars used by the Environment and Climate Change Canada

The Canadian weather radar network consists of 33 weather radars spanning Canada's most populated regions. Their primary purpose is the early detection of precipitation, its motion and the threat it poses to life and property.

<span class="mw-page-title-main">Lightning detector</span> Remote observation of lightning strikes

A lightning detector is a device that detects lightning produced by thunderstorms. There are three primary types of detectors: ground-based systems using multiple antennas, mobile systems using a direction and a sense antenna in the same location, and space-based systems. The first such device was invented in 1894 by Alexander Stepanovich Popov. It was also the first radio receiver in the world.

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

ARMOR Doppler weather radar is a C-Band, Dual-Polarimetric Doppler Weather Radar, located at the Huntsville International Airport in Huntsville, Alabama. The radar is a collaborative effort between WHNT-TV and the University of Alabama in Huntsville. Live data for the radar is only available to a limited audience, such as UAH employees and NWS meteorologists. All ARMOR data is archived at the National Space Science and Technology Center located on the UAH campus.

The AN/CPS-9 radar, the first radar specifically designed for meteorological use, was produced in the United States around 1949 and unveiled by the Air Weather Service in 1954.

The AN/APS-2, originally known as ASG, was a surface search radar developed by Philco originally for use in US Coast Guard blimps to detect German submarines. It proved better than several similar models then being built, and was ordered by the RAF Coastal Command where it was known as ASV Mark V. It was used primarily on British Liberator GR bombers, where they were instrumental in closing the Mid-Atlantic Gap and the subsequent destruction of the German U-boat fleet in May/June 1943.

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">Tornado vortex signature</span> Weather radar pattern

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">National Weather Service Lincoln, Illinois</span> Forecast office in central Illinois

National Weather Service Lincoln, Illinois also known as National Weather Service Central Illinois is a weather forecast office responsible for monitoring weather conditions for 35 counties in Central and Southeastern Illinois. The Central Illinois office initially consisted of two forecast offices in Peoria and Springfield until the current location in Lincoln became the sole local forecast office in 1995. Federal meteorology offices and stations in the region date back to the 19th century when the Army Signal Service began taking weather observations using weather equipment at the Springer Building in Springfield. Since that time the presence of the National Weather Service greatly increased with the installation of new weather radars, stations and forecast offices. The current office in Lincoln maintains a WSR-88D (NEXRAD) radar system, and Advanced Weather Interactive Processing System (AWIPS) that greatly improve forecasting in the region. Lincoln is in charge of weather forecasts, warnings and local statements as well as aviation weather.

<span class="mw-page-title-main">MESO-SAILS</span>

Multiple Elevation Scan Option for Supplemental Adaptive Intra-Volume Low-Level Scan, 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".

<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">SMART-R</span>

The Shared Mobile Atmospheric Research and Teaching Radar, colloquially known as SMART-R or SR, is a mobile Doppler weather radar platform operated and created by University of Oklahoma (OU) with aide from Texas A&M and Texas Tech University in 2001.

<span class="mw-page-title-main">Joint Polarization Experiment</span>

The Joint Polarization Experiment (JPOLE) was a test for evaluating the performance of the WSR-88D in order to modify it to include dual polarization. This program was a joint project of the National Weather Service (NWS), the Federal Aviation Administration (FAA), and the US Air Force Meteorological Agency (AFWA), which took place from 2000-2004. It has resulted in the upgrading of the entire meteorological radar network in the United States by adding dual polarization to better determine the type of hydrometeor, and quantities that have fallen.

References

  1. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 Whiton, Roger C.; al. (19 February 1998). "History of Operational Use of Weather Radar by U.S. Weather Services. Part I: The Pre-NEXRAD Era". Weather and Forecasting . 13 (2). American Meteorological Society: 219–243. doi: 10.1175/1520-0434(1998)013<0219:HOOUOW>2.0.CO;2 .
  2. S. G. Bigler; P. L. Hexter Jr.; F. E. Wells (November 1962). "The Radar Program of the U. S. Weather Bureau". Bulletin of the American Meteorological Society . 43 (11): 591–603. doi: 10.1175/1520-0477-43.11.591 . ISSN   0003-0007 . Retrieved 2021-09-04.
  3. 1 2 3 4 Chris Geelhart (Central Office in Illinois) (9 March 2011). "Brief History of National Weather Service Offices Past and Present". National Weather Service. Retrieved 5 April 2018.
  4. David Atlas; Banks, Harold C. (October 1951). "The interpretation of microwave reflections from rainfall". Journal of Meteorology . 8 (5): 271–282. doi: 10.1175/1520-0469(1951)008<0271:TIOMRF>2.0.CO;2 .