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TIFR Zero-Pressure Balloon Programme Crosses a Milestone


Affiliations
1 TIFR Balloon Facility, ECIL Post, Hyderabad 500 062, India
2 Tata Institute of Fundamental Research, Colaba, Mumbai 400 005, India
 

High-altitude scientific balloons offer unique opportunities to carry scientific payloads to stratospheric altitudes at a cost several orders of magnitude lower than the corresponding satellite missions. Balloon-borne payloads are easy to implement allowing quick experiment turn-around times and inexpensive reflights can be conducted as the payload is recovered most of the times. In addition, in situ and high-resolution spatial and temporal measurements of the earth’s atmosphere can be made that might not be feasible with satellites. They are also used as a testbed to prove technologies for future satellite missions. Scientific ballooning was initiated at the Tata Institute of Fundamental Research (TIFR), Mumbai in 1945, when scientific instruments were flown to stratospheric altitudes using a cluster of weather balloons for cosmic-ray research. The need to have balloons float at constant stratospheric altitudes for studies in astronomy led to the initiation of work on the design and fabrication of zero-pressure polyethylene (ZP) balloons at TIFR in 1956. Since then, several ZP balloon flights have been conducted for studies in astronomy, atmospheric science, astrobiology, balloon technology and space technology development, leading to several important scientific results. In 2018, the TIFR balloon programme crossed an important milestone of conducting more than 500 ZP balloon flights. This article presents recent advancements made in some areas of scientific ballooning and details of balloon experiments conducted in the past two decades.

Keywords

Cold Brittle Point, Gore, Satellite Missions, Scientific Payloads, Stratospheric Altitudes, Zero-Pressure Balloon.
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  • Redkar, R. T., Scientific ballooning in India. Indian J. Radio Space Phys., 1991, 20, 169–175.

  • Damle, S. V. and Joshi, M. N., Developments and advances in scientific balloon capability at the TIFR National Balloon Facility, Hyderabad. Adv. Space Res., 1998, 21(7), 941–948.

  • Gokhale, G. S., Menon, M. G. K. and Redkar, R. T., Stratospheric flights over tropical latitudes with polyethylene balloons of large volume. Proc. Indian Acad. Sci. Sect. A, 1966, 64(2), 57–63.

  • Suneel Kumar, B. et al., Mechanical properties of ANTRIX balloon film and fabrication of single cap large volume balloons. Adv. Space Res., 2008, 42, 1691–1697.

  • Manchanda, R. K., Scientific ballooning in India. Adv. Space Res., 2006, 37, 2015–2020.

  • Manchanda, R. K., High energy X-ray observations of NGC 5506.Adv. Space Res., 2006, 38, 1387–1392.

  • Manchanda, R. K., Characteristics and performance of thin LaBr3(Ce) crystal for hard X-ray astronomy. Adv. Space Res., 2011, 47, 30–36.

  • Manchanda, R. K., Current developments and future plans at NBF@Hyderabad and prospects for long duration balloon flights. Trans. JSASS Aerospace Technol. Jpn, 2010, 8(27), 55– 62.

  • Roy, J. et al., Performance of large area X-ray proportional counters in a balloon experiment. Exp. Astron., 2016, 42(2), 249–270.

  • Mookerjea, B. et al., Mapping of large scale 158 μm (CII) line emission: Orion A. Astron. Astrophys., 2003, 404(2), 569–578.

  • Kaneda, H. et al., Large-scale mapping of the massive starforming region RCW38 in the (CII) and PAH emission. Astron. Astrophys., 2013, 556, A92.

  • Arimura, S. et al., Wide-area mapping of 155 micron continuum emission from the Orion molecular cloud complex. Publ. Astron. Soc. Jpn., 2004, 56(1), 51–60.

  • Presenna Kumar, B. et al., High altitude balloon borne Lidar experiment for the study of aerosols and clouds. COSPAR, 2010, 38, 4055.

  • Pallamraju, D. et al., Day time wave characteristics in the mesosphere lower thermosphere region: results from the balloon-borne investigations of regional-atmospheric dynamics experiment. J. Geophys. Res. Space Phys., 2014, 119, 2229–2242.

  • Suresh Babu, S. et al., Free tropospheric black carbon aerosol measurements using high altitude balloon: Do BC layers build ‘their own homes’ up in the atmosphere? Geophys. Res. Lett., 2011, 38, L08803.

  • Gurubaran, S. et al., A high-altitude balloon experiment to probe stratospheric electric fields from low latitudes. Ann. Geophys., 2017, 35, 189–201.

  • Vernier, J. P. et al., The balloon measurement campaigns of the Asian tropopause aerosol layer. Bull. Am. Meterol. Soc., 2018, 99(5), 955–973.

  • Narlikar, J. V. et al., A balloon experiment to detect microorganisms in the outer space. Astrophys. Space Sci., 2003, 285, 555– 562.

  • Shivaji, S. et al., Janibacter hoylei sp. nov., Bacillus isronensis sp. nov. and Bacillus aryabhattai sp. nov., isolated from cryotubes used for collecting air from the upper atmosphere. Int. J. Syst. Evolution. Microbiol., 2009, 59, 2977–2986.

  • Suneel Kumar, B. et al., Development of ultra-thin polyethylene balloons for high altitude research up to mesosphere. J. Astronom. Instrum., 2014, 3(2), 1440002.

  • Nott, J. et al., Balloon aspects of StratEx world altitude record sky dive. In AIAA Balloon Systems Conference, Dallas, TX, USA, 22–26 June 2015.

  • Sinha, P. R. et al., Development of balloon-borne impactor payload for profiling free tropospheric aerosol. Aerosol Sci. Technol., 2019, 53(3), 1–38.


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  • TIFR Zero-Pressure Balloon Programme Crosses a Milestone

Abstract Views: 267  |  PDF Views: 109

Authors

D. Anand
TIFR Balloon Facility, ECIL Post, Hyderabad 500 062, India
B. Suneel Kumar
TIFR Balloon Facility, ECIL Post, Hyderabad 500 062, India
Devendra Ojha
Tata Institute of Fundamental Research, Colaba, Mumbai 400 005, India

Abstract


High-altitude scientific balloons offer unique opportunities to carry scientific payloads to stratospheric altitudes at a cost several orders of magnitude lower than the corresponding satellite missions. Balloon-borne payloads are easy to implement allowing quick experiment turn-around times and inexpensive reflights can be conducted as the payload is recovered most of the times. In addition, in situ and high-resolution spatial and temporal measurements of the earth’s atmosphere can be made that might not be feasible with satellites. They are also used as a testbed to prove technologies for future satellite missions. Scientific ballooning was initiated at the Tata Institute of Fundamental Research (TIFR), Mumbai in 1945, when scientific instruments were flown to stratospheric altitudes using a cluster of weather balloons for cosmic-ray research. The need to have balloons float at constant stratospheric altitudes for studies in astronomy led to the initiation of work on the design and fabrication of zero-pressure polyethylene (ZP) balloons at TIFR in 1956. Since then, several ZP balloon flights have been conducted for studies in astronomy, atmospheric science, astrobiology, balloon technology and space technology development, leading to several important scientific results. In 2018, the TIFR balloon programme crossed an important milestone of conducting more than 500 ZP balloon flights. This article presents recent advancements made in some areas of scientific ballooning and details of balloon experiments conducted in the past two decades.

Keywords


Cold Brittle Point, Gore, Satellite Missions, Scientific Payloads, Stratospheric Altitudes, Zero-Pressure Balloon.

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DOI: https://doi.org/10.18520/cs%2Fv120%2Fi11%2F1672-1678