Skip to main content
Log in

Characterization of rain heights due to 0° isotherm in tropical and subtropical climates: implication on rain-induced attenuation prediction

  • Original Paper
  • Published:
Theoretical and Applied Climatology Aims and scope Submit manuscript

Abstract

In this paper, the dynamics of the structure of the rain profile as related to the zero-degree isotherm height and the implications for attenuation prediction along the Earth-space propagation links at locations in Nigeria, a tropical region, and South Africa, a subtropical region, are presented. Five-year (January 2010–December 2014) precipitation data on board the Tropical Rainfall Measuring Mission (TRMM) satellite have been analyzed over some selected locations in the two regions. The influences of the zero-degree isotherm height on some observed weather parameters are also discussed. The result on the influence of air temperature on rain height hr shows a significant increase in the tropical environment as compared with those in the subtropics. However, when hr results are compared with those obtained using rain height as recommended by the International Telecommunication Union (ITU), there is a significant difference at the 0.01% unavailability of the signal in a year particularly at higher frequencies. Further comparison with the slant path attenuation at 0.01% unavailability of the signal in a year shows a slight deviation (between 1.04 and 2.13 dB) in rain height than those acquired using the measured rain height in the tropical locations. Nevertheless, the result is slightly less than those obtained using the measured rain height in the subtropical locations with the differences in dB between − 0.49 and − 1.18. The overall results will be useful for estimating the link budgeting for digital radio satellite broadcasting. It will also be applicable for radar propagation systems at higher-frequency bands in Nigeria and South Africa.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7

Similar content being viewed by others

References

  • Allnutt JE (1989) Satellite-to-ground radiowave propagation—theory, practice and system impact at frequencies above 1 GHz. Peter Peregrinus, London

    Google Scholar 

  • Ajayi GO, Barbaliscia F (1990) Prediction of attenuation due to rain: characteristics of the 0°C isotherm in temperate and tropical climates. Int J Satellite Communication 8(3):187–196. https://doi.org/10.1002/sat.4600080311

    Article  Google Scholar 

  • Ajayi GO, Feng S, Radicella SM, Reddy BM (eds) (1996) In: Handbook on radiopropagation related to satellite communications in tropical and subtropical countries. ICTP, Trieste

  • Brang Cheng (2007): QoS in weather impacted wireless and satellite networks", 2007 I.E. International Conference on Systems Man and Cybernetics, 10/2007

  • Falade JA, Adesanya SO, Akinyemi GA (2014) Variability of meteorological factors on surface refractive index over Mowe, a coastal area in Nigeria. Indian J Radio Space Physics 43:355–361

    Google Scholar 

  • Heymsfield GM, Geerts B, Tian L (2000) TRMM precipitation radar reflectivity profiles as compared with high-resolution airborne and ground-based radar measurements. J Appl Meteorol 39:2080–2102

    Article  Google Scholar 

  • Iguchi T, Kozu T, Meneghini R, Awaka J, Okamoto K (2000) Rain profiling algorithm for TRMM precipitation radar. J Appl Meteorol 39(12):2038–2052. https://doi.org/10.1175/1520-0450(2001)040<2038:RPAFTT>2.0.CO;2

    Article  Google Scholar 

  • Ippolito, L. J (1989). Propagation effects handbook for satellite systems designs. A summary of propagation impairments on 10 to 100 GHz satellite links with techniques for system design. National Aeronautics and Space Administration (NASA) Doc. Scientific and Technical Information Branch. 1082(4)

  • ITU-R P. 618–11 (2013) Propagation data and prediction methods required for the design of Earth–space telecommunication systems, Propagation in non-ionized media. International Telecommunication Union, Geneva

  • ITU-R P. 839–4, “Rain Height Model for Prediction Methods,” International Telecommunication Union, Geneva

  • Karmakar P.K (2011), “Rain attenuation and its application at microwaves”, microwave propagation and remote sensing atmospheric influences with models and applications, CRC press, Taylor and Francis Group

  • Kumar A, Sarkar SK (2007) Cloud attenuation and cloud noise temperature over some Indian eastern stations for satellite communication. Indian J Radio Space Physics 36(5):375–379

    Google Scholar 

  • Kummerow C, Barnes W, Kozu T, Shiue J, Simpson J (1998) The tropical rainfall measuring mission (TRMM) sensor package. J Atmos Ocean Technol 15(3):809–817

  • Mandeep JS (2008) Rain height statistics for satellite communication in Malaysia. J Atmos Sol Terr Phys 70(13):1617–1620. https://doi.org/10.1016/j.jastp.2008.06.005

    Article  Google Scholar 

  • Mandeep JS (2009) 0 °C isotherm height for satellite communication in Malaysia. Adv Space Res 43(6):984–989. https://doi.org/10.1016/j.asr.2008.09.013

    Article  Google Scholar 

  • Maral G, Bousquet M, Sun Z (2009) “Uplink, downlink and overall link performance; inter-satellite links”, satellite communications systems, 5th edn. Willey, University of Surrey, UK

    Google Scholar 

  • Mondal NC, Sarkar SK (2003) Rain height in relation to 0°C isotherm height for satellite communication over the Indian subcontinent. Theor Appl Climatol 76(1-2):89–104. https://doi.org/10.1007/s00704-003-0002-y

    Article  Google Scholar 

  • Nalinggam R, Susthitha Menon P, Singh MJ, Islam MT, Ismail W (2013) Development of rain attenuation model for Southeast Asia equatorial climate. IET Commun 7(10):1008–1014. https://doi.org/10.1049/iet-com.2012.0298

    Article  Google Scholar 

  • NASDA, 1999: TRMM PR algorithm instruction manual V1.0. Communications research laboratory, 52 pp. [Available from Communications Research Laboratory, 4-2-1 Nukui-kitamachi, Koganei-chi, Tokyo 184, Japan]

  • Nor Azian MA., Din J, Lam HY “Rain height information from TRMM precipitation radar for satellite communication in Malaysia.” Proceedings of the 2011 I.E. Int. conf. on Space Science and Commu., 12–13 July, 2011, pp. 73–76

  • Ojo JS, Omotosho TV (2013) Comparison of 1-min rain rate derived from TRMM satellite data and raingauge data for microwave applications in Nigeria. J Atmos Sol Terr Phys 102:17–25

  • Ojo JS (2014) Rain height statistics based on 0°c Isotherm height using TRMM precipitation data for Earth-space satellite links in Nigeria, ISRN Atmospheric sciences. Hindawi Publishing Corporation. https://doi.org/10.1155/2014/798289

  • Ojo JS, Falodun SE, Odiba O (2014a) 0°C isotherm height Distribution for Earth-space communication satellite links in Nigeria, Indian. J. Radio and Space Physics 43(3):225–234

    Google Scholar 

  • Ojo JS, Ojo OL, Joseph-Ojo CI (2014b) Rain height information from TRMM precipitation radar and micro rain radar for radio communication studies in Nigeria, 2014 I.E. 6th International Conference on Adaptive Science & Technology (ICAST), Ota. https://doi.org/10.1109/ICASTECH.2014.7068104

  • Ojo JS, Owolawi PA (2014a) Development of one-minute rain-rate and rain-attenuation contour maps for satellite propagation system planning in a subtropical country: South Africa. Adv Space Res 54(8):1487–1501. https://doi.org/10.1016/j.asr.2014.06.028

    Article  Google Scholar 

  • Ojo JS, Owolawi PA (2014b) Prediction of time-series rain attenuation based on rain rate using synthetic storm techniques over a subtropical region. Southern Africa Telecommunication Networks Applications Conference (SATNAC) 2014:66–71

    Google Scholar 

  • Smyth TJ, Illingworth AJ (1998) Radar estimates of rainfall rates at the ground in the bright and non-bright band event. Quarterly J Radar Meteorological Soc 124(551):2417–2434. https://doi.org/10.1002/qj.49712455112

    Article  Google Scholar 

  • South Africa Weather (SAW), 2014. http://www.southafrica .info/plantrip/travel_tips/questions /climate.htm

  • Steiner M, Houze RA Jr, Yuter SE (1995) Climatological characterization of three-dimensional storm structure from operational radar and rain gauge data. J Appl Meteorol 34(9):1978–2007. https://doi.org/10.1175/1520-0450(1995)034<1978:CCOTDS>2.0.CO;2

    Article  Google Scholar 

  • Thurai M, Deguchi E, Iguchi T, Okamoto K (2003) Freezing height distribution in the tropics. Int J Satell Commun Netw 21:533–545

    Article  Google Scholar 

  • Thurai M, Deguchi E, Okamoto K, Salonen E (2005) Rain height variability in the tropics. IEE Proceedings - Microwaves Antennas Propagation 152(1):17–23. https://doi.org/10.1049/ip-map:20041146

    Article  Google Scholar 

  • Yang X and Zhu L (2008) “Research on rain attenuation for ka-band satellite communication system”, 2008 ISECS International Colloquium on Computing Communication Control and Management. https://doi.org/10.1109/CCCM.2008.234

Download references

Acknowledgements

The authors will like to express their gratitude to the following organizations: NASA Goddard Space Flight, Centre Earth Enterprise Distributed Active Archive Centre (GES DAAC), South African Weather Stations, and Nigerian Meteorological Station for assessing the data used. One of the authors, JSO, also acknowledges one of his students—Omokaji Odiba.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to J. S. Ojo.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Ojo, J.S., Owolawi, P.A. Characterization of rain heights due to 0° isotherm in tropical and subtropical climates: implication on rain-induced attenuation prediction. Theor Appl Climatol 135, 331–340 (2019). https://doi.org/10.1007/s00704-018-2382-z

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00704-018-2382-z

Navigation