Impact of Cyclone Nilam on Tropical Lower Atmospheric Dynamics

• Published in: Advances in atmospheric sciences Vol. 33; no. 8; pp. 955 - 968
• Main Authors: Vinay Kumar, P., Dutta, Gopa, Ratnam, M. V., Krishna, E., Bapiraju, B., Rao, B. Venkateswara, Mohammad, Salauddin
• Format: Journal Article
• Language: English
• Published: Heidelberg Science Press 01.08.2016; Springer Nature B.V; Vignana Bharathi Institute of Technology, Hyderabad, TS 501301, India%National Atmospheric Research Laboratory, Gadanki, AP 517112, India%Jawaharlal Nehru Technological University, Hyderabad, TS 500085, India
• Subjects: Atmospheric Sciences; Cyclones; Earth and Environmental Science; Earth Sciences; Geophysics/Geodesy; Global positioning systems; GPS; Gravity waves; Humidity; Meteorology; Refractivity; Storms; Stratosphere; Tropopause; Troposphere; Turbulence; 低层; 大气动力学; 对流层顶; 惯性重力波; 折射率结构常数; 旋风; 气旋路径; 热带; India, Andhra Pradesh, Hyderabad; India, Andhra Pradesh, Gadanki; Bay of Bengal; tropical cyclone; convective process; inertia gravity waves; turbulence; momentum flux
• ISSN: 0256-1530; 1861-9533
• DOI: 10.1007/s00376-016-5285-x

A deep depression formed over the Bay of Bengal on 28 October 2012, and developed into a cyclonic storm. After landfall near the south coast of Chennai, cyclone Nilam moved north-northwestwards. Coordinated experiments were conducted from the Indian stations of Gadanki（13.5？N, 79.2？E） and Hyderabad（17.4？N, 78.5？E） to study the modification of gravity-wave activity and turbulence by cyclone Nilam, using GPS radiosonde and mesosphere–stratosphere–troposphere radar data. The horizontal velocities underwent large changes during the closest approach of the storm to the experimental sites. Hodograph analysis revealed that inertia gravity waves（IGWs） associated with the cyclone changed their directions from northeast（control time） to northwest following the path of the cyclone. The momentum flux of IGWs and short-period gravity waves（1–8 h） enhanced prior to, and during, the passage of the storm（±0.05 m2s-2and ±0.3 m2s-2, respectively）, compared to the flux after its passage. The corresponding body forces underwent similar changes, with values ranging between ±2–4m s-1d-1and ±12–15 m s-1d-1. The turbulence refractivity structure constant（C2n） showed large values below 10 km before the passage of the cyclone when humidity in the region was very high. Turbulence and humidity reduced during the passage of the storm when a turbulent layer at ～17 km became more intense. Turbulence in the lower troposphere and near the tropopause became weak after the passage of the cyclone.