Meteorology and Atmospheric Physics

, Volume 100, Issue 1, pp 207–215

Teleconnection mode between IOD and Northern Hemisphere tropospheric circulation and its mechanism

Authors

    • Jiangsu Key Laboratory of Meteorological DisasterNanjing University of Information Science and Technology
  • Q. Zhou
    • Jiangsu Key Laboratory of Meteorological DisasterNanjing University of Information Science and Technology
  • N. Liu
    • Key Laboratory of Marine Science and Numerical ModelingState Oceanic Administration
  • Q. Gao
    • Jiangsu Key Laboratory of Meteorological DisasterNanjing University of Information Science and Technology
    • Jiangsu Key Laboratory of Meteorological DisasterNanjing University of Information Science and Technology
Article

DOI: 10.1007/s00703-008-0304-9

Cite this article as:
Min, J., Zhou, Q., Liu, N. et al. Meteorol Atmos Phys (2008) 100: 207. doi:10.1007/s00703-008-0304-9

Summary

The teleconnection mode between IOD (Indian Ocean Dipole) and Northern Hemisphere tropospheric circulation and its mechanism are studied through GISST and NCEP/NCAR reanalysis data sets and by using diagnostic and theoretical methods and numerical simulations. The study shows that, in autumn, IOD is closely related with upper tropospheric geopotential height field in the Northern Hemisphere through teleconnection. It generates a Rossby wave train, starting from the northeast of India and ending in the east of Canada. The remote response time scale is about 2–3 months. The theory of planetary wave energy propagation can be used to explain its mechanism. It is found that the energy propagation of 1–3 latitudinal planetary wave numbers is the possible mechanism for the teleconnection between the IOD and tropospheric circulation. This teleconnection has been confirmed by further numerical experiments using the NCAR/CAM model, which demonstrates that IOD exerts a significant impact on the atmospheric circulations in the Northern Hemisphere.

Copyright information

© Springer-Verlag 2008