'Cyclonic' presentation slideshows

IoE 184 - The Basics of Satellite Oceanography. 8. Mesoscale variability and coastal pollution

Lecture 8 Mesoscale variability and coastal pollution. IoE 184 - The Basics of Satellite Oceanography. 8. Mesoscale variability and coastal pollution. This lecture includes the following topics:. Phytoplankton, the main contributor to ocean color: Passive tracer Active growing biomass.

855 views • 68 slides

HOW DOES AIR FLOW AROUND CYCLONIC AND ANTICYCLONIC CELLS?

HOW DOES AIR FLOW AROUND CYCLONIC AND ANTICYCLONIC CELLS?. CYCLONE ( LOW N). ANTI-CYCLONE. L. H. NORTHERN. L. H. SOUTHERN. 1) Pressure Gradient. 2) Coriolis Effect. CYCLONE ( LOW N). ANTI-CYCLONE. L. H. NORTHERN. L. H. SOUTHERN. 1) Pressure Gradient. 2) Coriolis Effect.

533 views • 47 slides

Role of mean state and local air-sea interaction on the propagation of intraseasonal oscillations

Role of mean state and local air-sea interaction on the propagation of intraseasonal oscillations. R. S. Ajayamohan Canadian Center for Climate Modelling and Analysis, Victoria, Canada. Collaborators: H. Annamalai, W. J. Merryfield, J. J. Luo, J. Hafner, T. Yamagata. Outline.

444 views • 34 slides

A Preliminary Study of Mesoscale Eddy effects on the Formation of the NPSTMW

ARGO 12-14 November 2003 Tokyo, Japan. A Preliminary Study of Mesoscale Eddy effects on the Formation of the NPSTMW. Aijun Pan & Qinyu Liu Physical Oceanography Lab. Ocean University of China ? Qingdao, P.R. China. Introduction 1. Pycnostad or thermostad Formation mechanism

416 views • 22 slides

Currents and Carbonate System in the Deep Black Sea

Currents and Carbonate System in the Deep Black Sea. James W. Murray School of Oceanography University of Washington Seattle, WA. Ankara Dec 5, 2006. Deep Currents using ARGO Profiling Floats (Korotaev, Oguz and Riser, 2006).

278 views • 17 slides

Bow Echoes

Bow Echoes. Bow Echo: radar-observed features. mesovortex. mesovortex. weak echo notch. apex of bow echo. bookend vortex. mid-level overhang. Houze et al. (BAMS 1989). Front-to-Rear Flow. All flows are system-relative. Ascending front-to-rear flow:

351 views • 13 slides

326 views • 10 slides

paoc.mit/labweb/lab9/gfd_9.htm

cyclonic. anti-cyclonic. geostrophic circulation with relative vorticity. leads to. frictional boundary layer flow from high to low pressure. y. ? divergence!!! ? vertical velocity. x. http://paoc.mit.edu/labweb/lab9/gfd_9.htm.

135 views • 1 slides