Kaushik Srinivasan

Apr 12, 2024 | agupubs.onlinelibrary.wiley.com | Kaushik Srinivasan |Mickaël D. Chekroun |James McWilliams

1 Introduction Turbulent flows in physical systems span a vast range of spatial and temporal scales; in the Earth's oceans, for example, mesoscale eddies, the dominant reservoir of kinetic energy in the ocean, have scales of O(100 km) whereas, small-scale three dimensional motions at the air-sea interface driven by a combination of surface heating/cooling, wind action and the Earth's rotation have scales of O(1m).

Mar 12, 2024 | journals.ametsoc.org | Roy Barkan |Kaushik Srinivasan |James McWilliams

Share Link Copy this link, or click below to email it to a friend Email this content or copy the link directly: The link was not copied. Your current browser may not support copying via this button.

Jan 15, 2024 | journals.ametsoc.org | Audrey Delpech |Roy Barkan |Kaushik Srinivasan |James McWilliams

Share Link Copy this link, or click below to email it to a friend or copy the link directly: The link was not copied. Your current browser may not support copying via this button.