ACPD Atmospheric Chemistry and Physics Discussions ACPD 1680-7375 Copernicus GmbH Göttingen, Germany 10.5194/acpd-3-1925-2003 Halogen Occultation Experiment (HALOE) and balloon-borne in situ measurements of methane in stratosphere and their relation to the quasi-biennial oscillation (QBO) Patra P. K. 1 Lal S. 2 Lal S. 2 Chand D. 3 Frontier Research System for Global Change, Yokohama 236 0001, Japan Physical Research Laboratory, Ahmedabad 380 009, India Max Planck Institute for Chemistry, 55020 Mainz, Germany 14 04 2003 3 2 1925 1947 This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. This article is available from http://www.atmos-chem-phys-discuss.net/3/1925/2003/acpd-3-1925-2003.html The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/3/1925/2003/acpd-3-1925-2003.pdf

Measurements of methane have been made from various observational platforms in the atmosphere. In this article, we have compared four high precision balloon-borne measurements from Hyderabad (17.5&deg; N), India in the period of 1987 and 1998 with a part of HALOE/UARS global observations available since 1991. All the balloon measurements correspond to boreal spring (March and April) but belong to different years. A comparison shows fairly good agreement with each other. The strongest effect of dynamical influence on methane vertical profiles is shown to be resulting from the quasi-biennial oscillation (QBO) in the stratosphere, and that has been consistently derived from both the measurement techniques. It is observed that the QBO signal in CH<sub>4</sub> anomaly exhibits interhemispheric asymmetry caused by the tropics to midlatitude circulation in the stratosphere. A mechanism is suggested to explain how and to what extent the methane vertical profiles over Hyderabad and higher latitudes could be modulated by the prevailing QBO winds in the tropics. We have also discussed how the same mechanism would affect ozone distribution in the stratosphere quite differently.