Impact of quasi-biennial oscillation on the inter-annual variability of the tropopause height and temperature in the tropics: A study using COSMIC/FORMOSAT-3 observations

被引:27
作者
Kumar, V. [1 ,2 ]
Dhaka, S. K. [1 ]
Reddy, K. K. [3 ]
Gupta, A. [1 ,2 ]
Prasad, S. B. Surendra [3 ]
Panwar, V. [1 ]
Singh, Narendra [4 ]
Ho, Shu-Peng [5 ]
Takahashi, M. [6 ]
机构
[1] Univ Delhi, Radio & Atmospher Phys Lab, Rajdhani Coll, Delhi 110007, India
[2] Univ Delhi, Dept Phys & Astrophys, Delhi 110007, India
[3] Yogi Vemana Univ, Dept Phys, Kadapa, Andhra Pradesh, India
[4] ARIES Nainital, Naini Tal, India
[5] Univ Corp Atmospher Res, COSMIC Program Off, Boulder, CO USA
[6] Univ Tokyo, Atmosphere & Ocean Res Inst, Tokyo 1138654, Japan
基金
美国国家科学基金会;
关键词
COSMIC/FORMOSAT-3; Remote sensing; QBO; Annual variation; GPS RADIO OCCULTATION; ANNUAL CYCLE; STRATOSPHERE; TROPOSPHERE; REGION;
D O I
10.1016/j.atmosres.2013.12.014
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The effect of quasi-biennial oscillation (QBO) on the temperature of cold point tropopause (T-CPT) and its height (H-CPT) is being investigated using radio occultation measurements by COSMIC/FORMOSAT-3. Observations comprising of 935,863 numbers of occultations have been used to study the zonal mean seasonal variability in T-CPT and H-CPT from January 2007 to December 2011. Results are shown over 30 degrees N-30 degrees S geographic latitudes. In general, T-CPT is found to be the coldest in February and the warmest in August H-CPT attains maximum height during December-February and minimum during July-August Interestingly, H-CPT shows maxima at off-equator region (around 20 degrees N or 20 degrees S) during all the seasons in both hemispheres. H-CPT at off-equatorial region, in reference to the equatorial region, is slightly higher (similar to 1.0 km) during winter as compared to monsoon season (similar to 0.5 km) in Northern Hemisphere (NH). Inter-annual variation in T-CPT and H-CPT found to be clearly influenced by the QBO. Westerly (easterly) phase generates warm (cold) T-CPT, which consequently results a decrease (increase) in H-CPT. It is concluded that QBO induces the changes in T-CPT by as much as 2 degrees C and in H-CPT by 0.5 km. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:62 / 70
页数:9
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