Download presentation
Presentation is loading. Please wait.
Published byAnnabel Atkins Modified over 9 years ago
1
El Nino Southern Oscillation
2
Oceanic Temperatures as a Function of ENSO (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.) Warm west, cold east Warm everywhere, but particularly in the central Pacific Warming erodes everywhere in response to upwelling
3
Oceanic Temperatures as a Function of ENSO (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
4
Oceanic Temperatures as a Function of ENSO (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
5
Oceanic Temperatures as a Function of ENSO (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
6
Southern Oscillation Index (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.) p diff = p(Tahiti) – p(Darwin)
7
Southern Oscillation Index (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.) El Nino: Warmer at Tahiti -> Lower SLP -> Negative SOI La Nina: Cooler at Tahiti -> Higher SLP -> Positive SOI
8
ENSO Monitoring Regions (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
9
Walker Circulation During La Nina Events (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.) Enhanced heating drives enhanced ascent Enhanced cooling drives enhanced descent
10
Walker Circulation During El Nino Events (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.) Enhanced heating drives enhanced ascent Weakened cooling drives substantially weakened descent
11
El Nino and the Australian Monsoon (Figure obtained from Ch. 3 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
12
El Niño and W. Hemisphere Hurricanes (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
13
NH Winter Impacts of El Niño (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
14
NH Summer Impacts of El Niño (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
15
NH Winter Impacts of La Niña (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
16
NH Summer Impacts of La Niña (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
17
Northern Hemispheric Pattern Modulation by ENSO (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
18
Delayed Oscillator Theory (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
19
Delayed Oscillator Theory (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
20
Western Pacific Oscillator Theory (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
21
Dynamical Model Forecasts of ENSO (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
22
Statistical Model Forecasts of ENSO (Figure obtained from Ch. 4 of An Introduction to Tropical Meteorology, 2 nd Edition. © 2011, COMET.)
Similar presentations
© 2024 SlidePlayer.com. Inc.
All rights reserved.