'Trade wind' diaporamas de présentation

918 views • 73 slides

734 views • 73 slides

370 Tropical

370 Tropical. Trade Wind Inversion. Trade Wind or Subtropical Inversion. The height of the base of this inversion varies from about 500 m at the eastern extremities of the subtropical highs to about 2000 m at the western and equatorial extremities.

853 views • 68 slides

370 Tropical

370 Tropical. Trade Wind Inversion. Trade Wind or Subtropical Inversion. The height of the base of this inversion varies from about 500 m at the eastern extremities of the subtropical highs to about 2000 m at the western and equatorial extremities.

744 views • 64 slides

551 Tropical

551 Tropical. Advanced Topics. Trade Wind Inversion. One starts with subsidence in the subtropics. But the subsidence is not zonally uniform: greater in the eastern side of the oceans.

474 views • 47 slides

ISLAND-SCALE CIRCULATIONS OF THE ISLAND OF HAWAII DURING HARP AND THE SUMMER OF 2004 Presented by

ISLAND-SCALE CIRCULATIONS OF THE ISLAND OF HAWAII DURING HARP AND THE SUMMER OF 2004 Presented by Yi-Leng Chen Department of Meteorology University of Hawaii at Manoa 2525 Correa Road Honolulu, HI 96822 Email: yileng@hawaii.edu November 2 9 , 2006, National Central University.

448 views • 44 slides

551 Tropical

551 Tropical. Advanced Topics. Trade Wind Inversion. One starts with subsidence in the subtropics. But the subsidence is not zonally uniform: greater in the eastern side of the oceans.

425 views • 42 slides

551 Tropical

551 Tropical. Advanced Topics. Trade Wind Inversion. One starts with subsidence in the subtropics. But the subsidence is not zonally uniform: greater in the eastern side of the oceans.

423 views • 42 slides

Atmospheric Physics I

Atmospheric Physics I. PHYS 621, Fall 2011 Dr. Zhibo Zhang Contact info: Phone: 410-455 - 6315 (office) Email: Zhibo.Zhang@umbc.edu Office hour: Friday, 3:30~4:30 or by appointment Course Website: UMBC Blackboard system &

548 views • 33 slides

MJO, ENSO, QBO, and Other Patterns

MJO, ENSO, QBO, and Other Patterns. Madden Julian Oscillation (MJO). Wavenumber-1 (possibly, wavenumber 2 at times) equatorially trapped Kelvin wave which is convectively coupled 1 st baroclinic mode atmospheric structure 30-60 day period Propagation ~5-10 ms -1 to east

564 views • 31 slides

551 Tropical

551 Tropical. Advanced Topics. Trade Wind Inversion. Trade Wind or Subtropical Inversion. The height of the base of this inversion varies from about 500 m at the eastern extremities of the subtropical highs to about 2000 m at the western and equatorial extremities.

306 views • 30 slides

MJO, ENSO, QBO, and Other Patterns

MJO, ENSO, QBO, and Other Patterns. Madden Julian Oscillation (MJO). Wavenumber-1 (possibly, wavenumber 2 at times) equatorially trapped Kelvin wave which is convectively coupled 1 st baroclinic mode atmospheric structure 30-60 day period Propagation ~5-10 ms -1 to east

294 views • 29 slides

THE GLOBAL CLIMATE

309 views • 19 slides

Validation Exercise

Validation Exercise. First: Where is the GDI expected to work?. GDI-BT r^2. In areas there the ECI is high. These often exclude cold current environments and areas that are too cool and dry such as the extratropics. Summer. ECI High in Summer.

254 views • 16 slides

Validation Exercise

Validation Exercise. First: Where is the GDI expected to work?. GDI-BT r^2. In areas there the ECI is high. These often exclude cold current environments and areas that are too cool and dry such as the extratropics. Summer. ECI High in Summer.

292 views • 16 slides

Validation Exercise

Validation Exercise. First: Where is the GDI expected to work?. GDI-BT r^2. In areas there the ECI is high. These often exclude cold current environments and areas that are too cool and dry such as the extratropics. Summer. ECI High in Summer.

166 views • 16 slides

Tong Lee NASA Jet Propulsion Laboratory, California Institute of Technology Michael McPhaden

Decadal variability in the Indo-Pacific ocean inferred from satellite data and ECCO assimilation. Tong Lee NASA Jet Propulsion Laboratory, California Institute of Technology Michael McPhaden NOAA Pacific Marine and Environmental Laboratory.

239 views • 13 slides