Travels of Law: Indian Ocean Itineraries

Ocean Currents Modeling along the Iranian Coastline of the Oman Sea and the Northern Indian Ocean

The Makran Coast (Iranian Coastline of the Oman Sea on the Northern Indian Ocean) plays an important role in country’s future navigation and trade due to its accessibility. In 2014, the Iranian Makran coastline was selected by the PMO to be studied as the Phase 6 in the series of Monitoring and Modelling Studies of Iranian Coasts with all disciplines being in investigated including currents. Al...

North Indian Ocean variability during the Indian Ocean dipole

1 Geophysical Fluid Dynamics Institute, Florida State University, Tallahassee, Florida, USA 2 Department of Aerospace Engineering Sciences, University of Colorado, Boulder, Colorado, USA 3 Department of Mathematics, Burapha University, Thailand Received: 26 March 2008 – Accepted: 8 April 2008 – Published: 9 June 2008 Correspondence to: J. Brown ([email protected]) Published by Copernicus Publ...

A Mathematical Model for Indian Ocean Circulation in Spherical Coordinate

In recent years, the Indian Ocean (IO) has been discovered to have a much larger impact on climate variability than previously thought. This paper reviews processes in which the IO is, or appears to be, actively involved. We begin the mathematical model with a pattern for summer monsoon winds. Three dimensional temperature and velocity fields are calculated analytically for the ocean forced by ...

An Indian Ocean dilemma: Sino-Indian rivalry and China’s strategic vulnerability in the Indian Ocean

This paper looks at the key strategic issues faced by China in the Indian Ocean within the context of growing Sino-Indian rivalry. It makes two basic arguments: first, that China has considerable strategic disadvantages in the Indian Ocean as compared with India; and second, that India has had more success than China in developing security relationships in the region. These propositions differ ...

Trade Potential And Among Indian Ocean Border Countries: Application Of The Gravity Model