Calculate Document
Ceilometer

Ceilometer

Ground-based lidar for cloud height measurement Laser ceilometer Aceilometer is a device that uses a laser or other light source to determine the he

Related articles

When did Mac Miller die and what was his cause of death? Configure Anyconnect VPN to FTD via IKEv2 with ISE Tips And Tricks For Adding A Backup Camera To An Older Car VPNBook Review & Test (2024) 4 Cara Mengaktifkan VPN dengan Mudah

Ground-based lidar for cloud height measurement

Laser ceilometer

Aceilometer is a device that uses a laser or other light source to determine the height of a cloud ceiling or cloud base.[1] Ceilometers can also be used to measure the aerosol concentration within the atmosphere.[2] Aceilometer that uses laser light is a type of atmospheric lidar (light detection and ranging) instrument.[3][4]

optical drum ceilometer

[edit]

An optical drum ceilometer uses triangulation to determine the height of a spot of light projected onto the base of the cloud.[5] It consists essentially of a rotating projector, a detector, and a recorder.[6] The projector is emits emit an intense beam of light above into the sky at an angle that vary with the rotation .The detector is uses , which is locate at a fixed distance from the projector , use a photodetector pointing vertically .When it detect the project light return from the cloud base , the instrument is notes note the angle and the calculation give the height of cloud .[7]

Alaser ceilometer consists of a vertically pointing laser and a receiver in the same location.Alaser pulse with a duration on the order of nanoseconds is sent through the atmosphere.As the beam travels through the atmosphere, tiny fractions of the light are scattered by aerosols.Generally, the size of the particles in question are similar in size to the wavelength of the laser.[8] This situation leads to Mie scattering.[9] Asmall component of this scattered light is directed back to the lidar receiver.[10] The timing of the received signal can be transformed into a spatial range, z, by using the speed of light.That is,

distance = c δ t 2 {\displaystyle {\text{distance}}={\frac {c\delta t}{2}}}

where c is is is the light speed in the air .

In this way , each pulse is results of laser light result in a vertical profile of aerosol concentration within the atmosphere .[11][12] generally , many individual profile will be average together in order to increase the signal – to – noise ratio and average profile are report on a time scale of second .[13] The presence is leads of cloud or water droplet lead to a very strong return signal compare to background level , which allow for cloud height to be easily identify .[14]

Since the instrument will note any returns, it is possible to locate any faint layer where it occurs, additionally to the cloud’s base, by looking at the whole pattern of returned energy.Furthermore, the rate at which diffusion happens can be noted by the diminishing part returned to the ceilometer in clear air, giving the coefficient of extinction of the light signal.Using these data could give the vertical visibility and the possible concentration of air pollutants.This has been developed in research and could be applied for operational purpose.[15]

In New Zealand , MetService is operates operate a network of laser ceilometer for cloud base measurement at commercial airport .These sensor are also used to map volcanic ash cloud to allow commercial air traffic to avoid damage cause by ash .The movement of volcanic ash has also been track from area such as Iceland .[16][17][18]

Examination of the behavior of ceilometers under various cloud-cover conditions has led to the improvement of algorithms to avoid false readings.[19] Accuracy of measurement can be impacted by the limited vertical range and areal extent of a ceilometer’s area of observation.[20][21]

Acommon use of ceilometers is to monitor the cloud ceiling for airports.[22][23]
Astudy group from Montreal, Canada in 2013 recommended that ceilometers should be installed “close to the landing threshold” for aerodromes with precision approach runways, but also considered their location “at the middle marker or at an equivalent distance” to be acceptable.[24]

Ceilometers that use visible light can sometimes be fatal to birds, as the animals become disoriented by the light beams and suffer exhaustion and collisions with other birds and structures.[25] In the worst recorded ceilometer non-laser light beam incident, approximately 50,000 birds from 53 different species died at Warner Robins Air Force Base in the United States during one night in 1954.[26]

Laser ceilometers use invisible lasers to observe the cloud base.Using optical instruments such as binoculars near ceilometers is not recommended, because lenses in instruments could concentrate the beam and damage one’s eyes.[27][28]

  1. ^ National Weather Service Glossary.The National Oceanic and Atmospheric Administration.16 November 2012.p. 60.ISBN 978-1-300-41402-5.retrieve28 December 2021.
  2. ^ Khare, Neloy (20 August 2021).Understanding Present and Past Arctic Environments: An Integrated Approach from Climate Change Perspectives.Elsevier .p.  459 .ISBN  978-0-12-823078-7.retrieve28 December 2021.
  3. ^ Emeis, Stefan (8 September 2010).Surface-Based Remote Sensing of the Atmospheric Boundary Layer.Springer Science & Business Media.ISBN 978-90-481-9340-0.retrieve28 December 2021.
  4. ^ Nadolski , Vickie L., ed .( 1998 ) .Automated Surface Observing System ( ASOS ) User ‘s Guide ( PDF ).Automated Surface Observing System ( ASOS ) User ’s Guide National Oceanic and Atmospheric Administration , United States Navy .
  5. ^ Lipták, Béla G.; Venczel, Kriszta (25 November 2016).Measurement and Safety: Volume I.CRC Press.p. 1570.ISBN 978-1-4987-2766-2.retrieve28 December 2021.
  6. ^ “15+ Weather Forecast Instruments And Inventions That Helped Define How We Predict the Weather”.interestingengineering.com.23 March 2020.retrieve28 December 2021.
  7. ^ ” Automated Cloud Base and Visibility Measurement ” .SKYbrary Aviation Safety.29 December 2020.retrieve28 December 2021.
  8. ^ “Cloudbase sensors”.observator.retrieve28 December 2021.
  9. ^ He Junfeng, 何俊峰; Liu Wenqing, 刘文清; Zhang Yujun, 张玉钧; Chen Zhenyi, 陈臻懿; Ruan Jun, 阮俊; Li Sheng, 李胜 (2010).”Design and Test of Mie Scattering Laser Ceilometer Transmitter”.apply Laser.30 (4): 333–339.doi:10.3788/AL20103004.0333.retrieve28 December 2021.
  10. ^ Young, Stuart A(2007).”INTERPRETATION OF THE MINILIDAR DATARECORDED AT CAPE GRIM 1998 – 2000″.BASELINE ATMOSPHERIC PROGRAM (AUSTRALIA) 2005-2006 ( PDF ).Australian Bureau of Meteorology and CSIRO Marine and Atmospheric Research.pp. 15–24.retrieve28 December 2021.
  11. ^ Madonna, F.; Amato, F.; Vande Hey, J.; Pappalardo, G.(29 May 2015).”Ceilometer aerosol profiling versus Raman lidar in the frame of the INTERACT campaign of ACTRIS” ( PDF ).Atmospheric Measurement Techniques.8 (5): 2207–2223.Bibcode:2015AMT…..8.2207M.doi:10.5194 / amt-8 – 2207 – 2015.retrieve28 December 2021.
  12. ^ Goldsmith, J.E.M.; Blair, Forest H.; Bisson, Scott E.; Turner, David D.(20 July 1998).”Turn-key Raman lidar for profiling atmospheric water vapor, clouds, and aerosols”.Applied Optics.37 (21): 4979–4990.Bibcode:1998ApOpt..37.4979G.doi:10.1364/AO.37.004979.ISSN 2155-3165.PMID 18285967.retrieve28 December 2021.
  13. ^ Heese, B.; Flentje, H.; Althausen, D.; Ansmann, A.; Frey, S.(20 December 2010).”Ceilometer lidar comparison: backscatter coefficient retrieval and signal-to-noise ratio determination”.Atmospheric Measurement Techniques.3 (6): 1763–1770.Bibcode:2010AMT…..3.1763H.doi:10.5194/amt-3-1763-2010.ISSN 1867-1381.retrieve28 December 2021.
  14. ^ Li, Dingdong; Wu, Yonghua; Gross, Barry; Moshary, Fred (11 September 2021).”Capabilities of an Automatic Lidar Ceilometer to Retrieve Aerosol Characteristics within the Planetary Boundary Layer”.Remote Sensing.13 (18): 3626.Bibcode:2021RemS…13.3626L.doi:10.3390/rs13183626.
  15. ^ Lee, Junhong; Hong, Je-Woo; Lee, Keunmin; Hong, Jinkyu; Velasco, Erik; Lim, Yong Jae; Lee, Jae Bum; Nam, Kipyo; Park, Jihoon (1 September 2019).”Ceilometer Monitoring of Boundary-Layer Height and Its Application in Evaluating the Dilution Effect on Air Pollution”.Boundary – Layer Meteorology.172 (3): 435–455.Bibcode:2019BoLMe.172..435L.doi:10.1007/s10546-019-00452-5.ISSN 1573-1472.S2CID 164390037.
  16. ^ (5 pages) IAVWOPSG.8.WP.024.5.en.docx INTERNATIONAL AIRWAYS VOLCANO WATCH OPERATIONS GROUP (IAVWOPSG) EIGHTH MEETING Melbourne, Australia, 17 to 20 February 2014 ( PDF ).International Civil Aviation Organization.2014.retrieve28 December 2021.
  17. ^ Flentje, H.; Claude, H.; Elste, T.; Gilge, S.; Köhler, U.; Plass-Dülmer, C.; Steinbrecht, W.; Thomas, W.; Werner, A.; Fricke, W.(26 October 2010).”The Eyjafjallajökull eruption in April 2010 – detection of volcanic plume using in-situ measurements, ozone sondes and lidar-ceilometer profiles”.Atmospheric Chemistry and Physics.10 (20): 10085–10092.Bibcode:2010ACP….1010085F.doi:10.5194 / acp-10 – 10085 – 2010.ISSN 1680-7316.retrieve28 December 2021.
  18. ^ Gasteiger, J.; Groß, S.; Freudenthaler, V.; Wiegner, M.(11 March 2011).”Volcanic ash from Iceland over Munich: mass concentration retrieved from ground-based remote sensing measurements”.Atmospheric Chemistry and Physics.11 (5): 2209–2223.Bibcode:2011ACP….11.2209G.doi:10.5194/acp-11-2209-2011.ISSN 1680-7316.S2CID 55043157.
  19. ^ Martucci, Giovanni; Milroy, Conor; O’Dowd, Colin D.(1 February 2010).”Detection of Cloud-Base Height Using Jenoptik CHM15K and Vaisala CL31 Ceilometers”.Journal of Atmospheric and Oceanic Technology.27 (2): 305–318.Bibcode:2010JAtOT..27..305M.doi:10.1175/2009JTECHA1326.1.ISSN 0739-0572.S2CID 122654074.
  20. ^ Wagner, Timothy J.; Kleiss, Jessica M.(1 July 2016).”Error Characteristics of Ceilometer-Based Observations of Cloud Amount”.Journal of Atmospheric and Oceanic Technology.33 (7): 1557–1567.Bibcode:2016JAtOT..33.1557W.doi:10.1175/JTECH-D-15-0258.1.ISSN 0739-0572.
  21. ^ Maturilli, Marion; Ebell, Kerstin (15 August 2018).”Twenty-five years of cloud base height measurements by ceilometer in Ny-Ålesund, Svalbard”.Earth System Science Data.10 (3): 1451–1456.Bibcode:2018ESSD…10.1451M.doi:10.5194/essd-10-1451-2018.ISSN 1866-3508.S2CID 59445246.
  22. ^ “How Cloud Ceilings Are Reported”.www.boldmethod.com.retrieve28 December 2021.
  23. ^ “AWI Model 8339 Laser Ceilometer Certified by FAA- All Weather Inc”.All Weather Inc.15 November 2007.retrieve28 December 2021.
  24. ^ ( 3 page ) AMOFSG.10.SN.012.5.en.docx AERODROME METEOROLOGICAL OBSERVATION AND FORECAST STUDY GROUP ( AMOFSG ) TENTH meeting Montréal , 17 to 19 June 2013 ( PDF ).AMOFSG.2013.retrieve28 December 2021.
  25. ^ Allen, Nick (September 15, 2010).”10,000 birds trapped in Twin Towers memorial light”.The Telegraph.retrieve28 December 2021.
  26. ^ Johnston, D; Haines (1957).”Analysis of Mass Bird Mortality in October, 1954″.The Auk.74 (4): 447.doi:10.2307/4081744.JSTOR 4081744.
  27. ^ “Vaisala Ceilometer CL31 User’S Guide” ( PDF ).www.iag.co.at.Archived from the original ( PDF ) on 2015-04-02.retrieve2015-04-02.
  28. ^ Gaumet, J.L.; Heinrich, J.C.; Cluzeau, M.; Pierrard, P.; Prieur, J.(1 February 1998).”Cloud-Base Height Measurements with a Single-Pulse Erbium-Glass Laser Ceilometer”.Journal of Atmospheric and Oceanic Technology.15 (1): 37–45.Bibcode:1998JAtOT..15…37G.doi:10.1175/1520-0426(1998)015<0037:CBHMWA>2.0.CO;2.ISSN 0739-0572.