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Mesonet

From Wikipedia, the free encyclopedia
Network of weather and environment monitoring stations

Aweather map consisting of astation model plot ofOklahoma Mesonet data overlaid withWSR-88D weather radar data depicting possiblehorizontal convective rolls as a potential contributing factor in the incipient3 May 1999 tornado outbreak[1] A mobile mesonet also documentedtornadicsupercells and their immediate environments during this event.[2]

Inmeteorology andclimatology, amesonet, portmanteau of mesoscale network, is a network ofautomatedweather and, often also includingenvironmental monitoring stations, designed to observemesoscale meteorological phenomena and/ormicroclimates.[3][4]

Dry lines,squall lines, andsea breezes are examples of phenomena observed by mesonets. Due to the space and time scales associated with mesoscale phenomena and microclimates, weather stations comprising a mesonet are spaced closer together and report more frequently thansynoptic scale observing networks, such as theWMO Global Observing System (GOS) and USASOS. The term mesonet refers to the collective group of these weather stations, which are usually owned and operated by a common entity. Mesonets generally recordin situsurface weather observations but some involve other observation platforms, particularly vertical profiles of theplanetary boundary layer (PBL).[5] Other environmental parameters may includeinsolation and various variables of interest to particular users, such as soil temperature or road conditions (the latter notable inRoad Weather Information System (RWIS) networks).

The distinguishing features that classify a network of weather stations as a mesonet are station density and temporal resolution with sufficiently robust station quality. Depending upon the phenomena meant to be observed, mesonet stations use a spatial spacing of 1 to 40 kilometres (0.6 to 20 mi)[6] and report conditions every 1 to 15 minutes.Micronets (seemicroscale andstorm scale), such as in metropolitan areas such asOklahoma City,[7]St. Louis, andBirmingham UK, are denser in spatial and sometimes temporal resolution.[8]

Purpose

[edit]

Thunderstorms and otheratmospheric convection, squall lines, drylines,[9] sea and land breezes,mountain breeze and valley breezes,mountain waves,mesolows andmesohighs,wake lows,mesoscale convective vortices (MCVs),tropical cyclone andextratropical cyclonerainbands,macrobursts,gust fronts andoutflow boundaries,heat bursts,urban heat islands (UHIs), and other mesoscale phenomena, as well as topographical features, can causeweather andclimate conditions in a localized area to be significantly different from that dictated by the ambient large-scale conditions.[10][11] As such, meteorologists must understand these phenomena in order to improve forecast skill. Observations are critical to understanding the processes by which these phenomena form, evolve, and dissipate.

The long-term observing networks (ASOS,AWOS, COOP), however, are too sparse and report too infrequently for mesoscale research and forecasting. ASOS and AWOS stations are typically spaced 50 to 100 kilometres (30 to 60 mi) apart and report only hourly at many sites (though over time the frequency of reporting has increased, down to 5–15 minutes in the 2020s at major sites). TheCooperative Observer Program (COOP) database consists of only daily reports recorded manually. That network, like the more recentCoCoRaHS, is large but both are limited in reporting frequency and robustness of equipment. "Mesoscale" weather phenomena occur on spatial scales of a few to hundreds of kilometers and temporal (time) scales of minutes to hours. Thus, an observing network with finer temporal and spatial scales is needed for mesoscale research. This need led to the development of the mesonet.

Mesonet data is directly used by humans for decision making, but also boosts the skill ofnumerical weather prediction (NWP) and is especially beneficial for short-range mesoscale models. Mesonets, along withremote sensing solutions (data assimilation ofweather radar,weather satellites,wind profilers), allow for much greater temporal and spatial resolution in a forecast model. As theatmosphere is achaoticnonlineardynamical system (i.e. subject to theButterfly effect), this increase in data increases understanding ofinitial conditions and boostsmodel performance. In addition to meteorology and climatology users,hydrologists,foresters, wildland firefighters, transportation departments, energy producers and distributors, other utility interests, and agricultural entities are prominent in their need for fine scale weather information. These organizations operate dozens of mesonets within the US and globally. Environmental, outdoor recreational,emergency management andpublic safety, military, and insurance interests also are heavy users of mesonet information.

In many cases, mesonet stations may, by necessity or sometimes by lack of awareness, be located in positions where accurate measurements may be compromised. For instance, this is especially true ofcitizen science andcrowdsourced data systems, such as the stations built forWeatherBug's network, many of which are located on school buildings. TheCitizen Weather Observer Program (CWOP) facilitated by the USNational Weather Service (NWS) and other networks such as those collected byWeather Underground help fill gaps with resolutions sometimes meeting or exceeding that of mesonets, but many stations also exhibit biases due to improper siting, calibration, and maintenance. These consumer grade "personal weather stations" (PWS) are also less sensitive and rigorous than scientific grade stations. The potential bias that these stations may cause must be accounted for when ingesting the data into a model, lest the phenomenon of "garbage in, garbage out" occur.

Operations

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Kentucky Mesonet station WSHT nearMaysville inMason County

Mesonets were born out of the need to conduct mesoscale research. The nature of this research is such that mesonets, like the phenomena they were meant to observe, were (and sometimes still are) short-lived and may change rapidly. Long-term research projects and non-research groups, however, have been able to maintain a mesonet for many years. For example, the U.S. ArmyDugway Proving Ground inUtah has maintained a mesonet for many decades. The research-based origin of mesonets led to the characteristic that mesonet stations may be modular and portable, able to be moved from onefield program to another. Nonetheless, most large contemporary mesonets or nodes within consist of permanent stations comprising stationary networks. Some research projects, however, utilize mobile mesonets. Prominent examples include theVORTEX projects.[12][13] The problems of implementing and maintaining robust fixed stations are exacerbated by lighter, compact mobile stations and are further worsened by various issues related when moving, such as vehicleslipstream effects, and particularly during rapid changes in the ambient environment associated with traversingsevere weather.[14]

Whether the mesonet is temporary or semi-permanent, each weather station is typically independent, drawing power from abattery andsolar panels. An on-board computer records readings from several instruments measuringtemperature,humidity,windspeed anddirection, andatmospheric pressure, as well assoil temperature andmoisture, and other environmental variables deemed important to the mission of the mesonet,solar irradiance being a common non-meteorological parameter. The computer periodically saves these data to memory, typically usingdata loggers, and transmits the observations to a base station viaradio,telephone (wireless, such ascellular orlandline), orsatellite transmission. Advancements incomputer technology andwireless communications in recent decades made possible the collection of mesonet data in real-time. Some stations or networks report usingWi-Fi and grid powered with backups for redundancy.

The availability of mesonet data in real-time can be extremely valuable to operational forecasters, and particularly fornowcasting,[15] as they can monitor weather conditions from many points in their forecast area. In addition to operational work, and weather, climate, and environmental research, mesonet and micronet data are often important inforensic meteorology.[16]

History

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Three-daybarograph of the type used by theMeteorological Service of Canada

Early mesonets operated differently from modern mesonets. Each constituent instrument of the weather station was purely mechanical and fairly independent of the other sensors. Data were recorded continuously by an inked stylus that pivoted about a point onto a rotating drum covered by a sheath of graphed paper called a trace chart, much like a traditionalseismograph station. Data analysis could occur only after the trace charts from the various instruments were collected.

One of the earliest mesonets operated in the summer of 1946 and 1947 and was part of a field campaign calledThe Thunderstorm Project.[17] As the name implies, the objective of this program was to better understand thunderstorm convection. The earliest mesonets were typically funded and operated by government agencies for specific campaigns. In time, universities and other quasi-public entities began implementing permanent mesonets for a wide variety of uses, such as agricultural or maritime interests. Consumer grade stations added to the professional grade synoptic and mesoscale networks by the 1990s and by the 2010s professional grade station networks operated by private companies and public-private consortia increased in prominence. Some of these privately implemented systems are permanent and at fixed locations, but many also service specific users and campaigns/events so may be installed for limited periods, and may also be mobile.

The first known mesonet was operated by Germany from 1939 to 1941. Early mesonets with project based purposes operated for limited periods of time from seasons to a few years. The first permanently operating mesonet began in the United States in the 1970s with more entering operation in the 1980s-1990s as numbers gradually increased preceding a steeper expansion by the 2000s. By the 2010s there was also an increase in mesonets on other continents. Some wealthy densely populated countries also deploy observation networks with the density of a mesonet, such as theAMeDAS in Japan. The US was an early adopter of mesonets, yet funding has long been scattered and meager. By the 2020s declining funding atop the earlier scarcity and uncertainty of funding was leading to understaffing and problems maintaining stations, the closure of some stations, and the viability of entire networks threatened.[18]

Mesonets capable of being moved for fixed station deployments in field campaigns came into use in the US by the 1970s[19] and fully mobile vehicle-mounted mesonets became fixtures of large field research projects following the field campaigns of Project VORTEX in 1994 and 1995, in which significant mobile mesonets were deployed.

Significant mesonets

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The following table is an incomplete list of mesonets operating in the past and present:

Years of operationName of Network, PlaceSpacingNo. of Stations
(Year)
Objectives
1939-41Lindenberger Böennetz [de],Lindenberg [de],Tauche, Germany3–20 km (1.9–12.4 mi)19-25research on convective hazards, including squall lines and wind gusts, to aviation[11]
1940Maebashi, Japan8–13 km (5.0–8.1 mi)20
(1940)
research on convective hazards to aviation, examined structure of thunderstorms[11]
1941Muskingum basin,Ohio10 km (6.2 mi)131
(1941)
rainfall andrunoff research[11]
1946The Thunderstorm Project,Florida1 mi (1.6 km)50
(1946)
thunderstormconvection research[20]
1947The Thunderstorm Project, Ohio2 mi (3.2 km)58
(1947)
thunderstorm convection research[20]
1960New Jersey10 km (6.2 mi)23
(1960)
research on mesoscale pressure systems[11]
1960Fort Huachuca, Arizona20 km (12 mi)28
(1960)
Army operations (military meteorology) research[11]
1961Fort Huachuca, Arizona3 km (1.9 mi)17
(1961)
research on influence oforography[11]
1961–PresentDugway Proving Ground,Utah9 mi (14 km)26air quality modeling and other desert area research
1961Flagstaff, Arizona8 km (5.0 mi)43
(1961)
cumulonimbus convection research[11]
1961National Severe Storms Project (NSSP), Southern Plains US20 km (12 mi)36
(1961)
research on structure of severe storms[11][21]
1962National Severe Storms Project (NSSP), Southern Plains US60 km (37 mi)210
(1962)
research on squall lines and pressure jumps[11]
1961–1980s[22]NSSL mesonetwork and mesometeorological rawinsonde networks, Oklahoma<6-17 mi (<9–28 km) surface, 18-53 mi (30–85 km) upper (1966-1970)30-61 surface, 8-11 upper (1966-1970)primarily convection and dryline research in partnership with AF and Army, with focus in some years on aviation and particularly airport operations; annual field projects included varying number and spatial density of seasonal surface and upper air stations combined with radar and aircraft observations plus instrumented tower, leading to evolution of storm scale networks[23][24] and automated networks (e.g. NSSL Surface Automated Mesonetwork); other research projects increasingly arose in 70s-80s
1972–PresentEnviro-Weather,Michigan (now also adjacent sections ofWisconsin)Varies81agriculturally centered; archive, varies from 5-60 min observations[25]
1976-1982
1982-1987
NCAR Portable Automated Mesonet I
NCAR Portable Automated Mesonet II
30[19]
≈200[26]
research networks
1981–PresentNebraska Mesonet,NebraskaVaries69
(2018)
originally agriculturally centered now multipurpose; archive, near real-time observations[27][28][29]
1983–PresentSouth Dakota Mesonet,South DakotaVaries27archive, real-time 5 min observations[30]
1984-1986+FAA-Lincoln Laboratory Operational Weather Studies (FLOWS)30aviation research network focused on low-level wind shear and microburst hazards with radar (TDWR) and other detection systems that becameLLWAS[31]
1986–PresentKansas Mesonet,KansasVaries72archive, real-time observations[32]
1986–PresentArizona Meteorological Network (AZMET),ArizonaVaries27agriculturally centered; archive, real-time observations, 15 min - 1 hr[33]
1988–PresentWashington Mesonet/AgWeatherNet,WashingtonVaries177multi-network system (comprehensive monitoring, agricultural focused); archive, real-time observations, 5 and 15 min[34][35]
1989–PresentOhio Agricultural Research and Development Center (OARDC) Weather System,OhioVaries17agriculturally centered; archive, hourly observations[36]
1990–PresentNorth Dakota Agricultural Weather Network (NDAWN),North Dakota (also adjacent areas of NW-Minnesota and EasternMontana)Varies91 kilometres (57 mi)agriculturally centered; archive, real-time observations[37][38]
1991–PresentOklahoma Mesonet,OklahomaVaries121comprehensive monitoring; archive, real-time observations[39][40]
1991–PresentGeorgia Automated Weather Network (AEMN),GeorgiaVaries82agriculture andhydrometeorology; archive, real-time observations, 15 min[41][42]
1992–Present[43]Colorado Agricultural Meteorological Network (CoAgMet),Coloradoagriculturally centered; 5 min data, archived[44]
1993–PresentMissouri Mesonet,MissouriVaries35agriculturally centered; archive, real-time observations at 21 stations[45][46]
1994–PresentWeatherBug (AWS), across United StatesVaries>8,000 **real-time observations for schools and television stations; collection of multiple mesonets, each typically centered around a host television station'smedia market[47][48]
1997–PresentFlorida Automated Weather Network (FAWN),FloridaVaries42agriculturally-centered; archive, real-time[49][50]
1999–PresentWest Texas Mesonet,West TexasVaries63+archive, real-time observations[51][52]
2001–PresentIowa Environmental Mesonet,IowaVaries469*archive, real-time observations[53][54]
-PresentWeatherFlow, global but concentrated in USVaries450+ mesonet stations in proprietary network; 27,000 in total * **real-time and archive for variety of purposes, proprietary but reports to public forecasters and numerical modeling systems; operates specialty mesonets and offers PWSs[55]
2002–PresentSolutions Mesonet,Eastern CanadaVaries600+ *archive, real-time observations[56]
2002–PresentWestern Turkey Mesonet,TurkeyVaries206+nowcasting, hydrometeorology[57]
2003–PresentDelaware Environmental Observing System (DEOS),DelawareVaries57archive, real-time observations[58][59]
2004–PresentSouth Alabama Mesonet (USA Mesonet),AlabamaVaries26archive, real-time observations[60]
2004-2010Foothills Climate Array (FCA), southernAlberta10 km (6.2 mi) average300research on spatial-temporal meteorological variation, and onweather andclimate model performance, across adjoiningmountain,foothills, andprairie topographies[61]
2007–PresentKentucky Mesonet,KentuckyVaries82archive, real-time observations[62][63][64]
2007–PresentMount Washington Regional Mesonet,New Hampshire18
(2022)
archive, near-real time observations primarily for orography, operated byMount Washington Observatory[65][66][67]
2008–PresentQuantum Weather Mesonet,St. Louis metropolitan area, MissouriVaries (average ~5 miles (8.0 km))100 (proprietary)utility and nowcasting; archive, real-time observations[68]
-PresentNorth Carolina ECONet,North CarolinaVaries99archive, real-time observations[69]
2010–PresentWeather Telenatics,North AmericaVaries(proprietary)real-time and archived, proprietary; operates micronets, focused on ground transportation and airports but also serves other uses[70]
2012–PresentBirmingham Urban Climate Laboratory (BUCL) Mesonet,Birmingham UK3 per 1 km2 (0.4 sq mi)24urban heat island (UHI) monitoring[71][72]
2015–PresentNew York State Mesonet,New YorkVaries, averages 20 miles (32 km)126real-time observations, improved forecasting[73]
2016–PresentTexMesonet,TexasVaries100 in network; 3,151 total * **hydrometeorology andhydrology focused network operated by the Texas Water Development Board, plus network of networks; some real-time observations, archival[74]
-PresentNew Jersey Weather & Climate Network (NJWxNet),New JerseyVaries66real-time observations[75]
-PresentKeystone Mesonet,PennsylvaniaVariesreal-time observations, archived; variety of uses, network of networks[76]
-PresentCape Breton Mesonet,Cape Breton Island, with some stations inNewfoundland,Prince Edward Island, and mainlandNova ScotiaVaries141+real-time observations, with archived data available.[77]
2019–presentCOtL (Conditions Over the Landscape) Mesonet,South Australiaagriculturally focused with a particular emphasis on monitoring amenability of weather conditions for crop spraying; a merger of Mid North Mesonet that began operating in 2019 and Riverland & Mallee Mesonet which began in 2021 with additional networks anticipated[78]
≈2020–PresentUmbria region mesonet,Umbria,Central ItalyVariesnetwork of preexisting networks emerging since 2020 in part to monitor complex topography but with various purposes for constituent networks[79]
2022–PresentMaryland Mesonet,Maryland, USAVaries72 planned (2022)

9 operational (2024)

A network that will eventually total 72 stations across Maryland to promote: public safety,[80] transportation, agriculture, climate, and K-12 science. The program is managed by the University of Maryland,[81] with significant input from state and local government agencies, and local partner organizations.
2022–PresentHawai'i Mesonet,Hawaiian IslandsVaries>95
(2022)
near real-time observations with archives,[82] for a variety of weather and climate uses designed to measure the stark microclimates ofHawaii[83] and as an expansion to local micronets such as HaleNet, HavoNet, HIPPNET, and CraterNet[84]
In developmentWisconsin Environmental Mesonet (Wisconet), Wisconsin90near real-time observations with archives, agriculturally focused[85]

* Not all stations owned or operated by network.
** As these are private stations, althoughQA/QC measures may be taken, these may not be scientific grade, and may lack proper siting, calibration, sensitivity, durability, and maintenance.

Although not labeled a mesonet, theJapan Meteorological Agency (JMA) also maintains a nationwide surface observation network with the density of a mesonet. JMA operatesAMeDAS, consisting of approximately 1,300 stations at a spacing of 17 kilometres (11 mi). The network began operating in 1974.[86]

See also

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References

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  2. ^Markowski, Paul M. (2002)."Mobile Mesonet Observations on 3 May 1999".Weather Forecast.17 (3):430–444.Bibcode:2002WtFor..17..430M.doi:10.1175/1520-0434(2002)017<0430:MMOOM>2.0.CO;2.
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