Upwelling associated with ENSO events

Slides:



Advertisements
Similar presentations
Increased Storm Activity around the Globe.
Advertisements

Blow to the west across the tropical pacificTrade winds blow to the west across the tropical pacific Winds pile up warm water in the west pacific so the.
El Niño- Southern Oscillation
El Nino El Nino is hot air over hot water, which causes warm winds El Nino means boy in Spanish and it causes wet period in Midwestern US.
El Niño. What is El Niño? A shift in ocean current direction and water temperature El Niño: the ocean part: Warm phase of ENSO: El Niño - Southern Oscillation.
Estimate the latitude where warm El Niño water is located.
El Niño & La Niña.
El Niño.
El Niño El Niño is a variation in the ocean and atmospheric temperatures in the Pacific Ocean. When the ocean temperature increases it causes ocean currents.
El Niño. How do ocean currents affect weather and climate? Oceans store and transport heat. – High heat capacity – Stores and transports energy from the.
Ocean Currents
El Nino, La Nina, and their Affects in Oklahoma. El Nino Conditions Warming of central and eastern equatorial Pacific waters Trade wind differences –
El Nino Refers to a weak, warm current appearing annually around Christmas time along the coast of Ecuador and Peru and lasting only a few weeks to a month.
Class #16 Monday, October 4, 2010 Class #16: Monday, October 4 Chapter 8 Oceanography and El Niño/La Niña/ENSO 1.
El Niño - Southern Ocean Oscillation. El Niño-Southern Oscillation is a periodic change in the atmosphere and ocean of the tropical Pacific region. El.
Understanding El Nino and La Nina Aim: To understand the what this weather phenomena is and what conditions it brings (A.K.A – To understand a bloody difficult.
Do Now; Are there weather patterns that influence places thousands of miles away?
OCEAN INTERACTIONS WITH THE ATMOSPHERE Niki Henzel & Ron Gabbay.
Water and Wind Unit Chapter 13 Sections 2 & 3 Pages
El Nino and La Nina opposite phases of the El Niño-Southern Oscillation (ENSO) cycle. The ENSO cycle describes the changes in temperature between the ocean.
El Niño & La Niña. THREE CIRCULATIONS OF THE OCEANS Normal circulation (Walker circulation) El Nino circulation La Nina circulation.
Ocean Circulation Recall from last lecture that differential heating of the earth, along with the effects of the rotation of the globe cause generally.
Ocean Currents Chapter 5 Notes.
 Abnormally high surface ocean temperatures off the coast of South America  Causes unusual weather patterns across the globe El Nino.
El Niňo. El Nińo: A significant increase in sea surface temperature over the eastern and central equatorial Pacific that occurs at irregular intervals,
El Niño – The Christ Child (in Spanish)
1 NORMAL Normally, trade winds blow warm surface water toward the western Pacific. This causes the thermocline to rise near the surface in the eastern.
Much of the work that follows is straight from (or slightly modified) notes kindly made available by Jenny Pollock NCG and or spk (?)…. Nice to have a.
Lecture 9: Air-Sea Interactions EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p ; Ch. 16, p ; Ch. 17, p
Anomalous Behavior Unit 3 Climate of Change InTeGrate Module Cynthia M. Fadem Earlham College Russian River Valley, CA, USA.
Ocean Current s.  Warm currents flow away from the equator.  Cold currents flow toward the equator. Ocean Currents.
Normal Conditions The trade winds move warm surface water towards the western Pacific. Cold water wells up along the west coast of South America (the Peru.
Currents & Climate Ch Warm-water currents i.e. Gulf Stream Creates mild climate at high latitudes such as British Isles (much warmer than Newfoundland.
El Nino and La Nina. er/environment/environment-natural- disasters/landslides-and-more/el-nino.htmlhttp://video.nationalgeographic.com/video/play.
The ENSO Cycle Naturally occurring phenomenon – El Nino / Southern Oscillation (ENSO) Cycle Equatorial Pacific fluctuates between warmer-than-average.
ENSO El Niño—Southern Oscillation  El Niño (Spanish for “the Child” in reference to baby Jesus) = warm surface current in equatorial eastern Pacific.
Non El Niño Years The easterly trade winds of the tropics drag the surface waters of the eastern Pacific away from the coastlines of the Americas.easterly.
Recap Use the following graphs to explain what we discussed last lesson regarding frequency.
El Nino WORLD AT RISK Learning Intentions:
El Niño–Southern Oscillation (ENSO): What is it?
Climate Phenomena.
El Niño: A temperature anomaly
El Niño and La Niña.
Ocean/Air interaction
Ocean Currents & Global Climates
El Nino.
KUDAKWASHE KELVIN CHIKUKWA R169999D
El Nino.
El Nino.
El Niño and La Niña.
El Niño / Southern Oscillation (ENSO)
Differential Heating – Specific Heat
EL NINO Figure (a) Average sea surface temperature departures from normal as measured by satellite. During El Niño conditions upwelling is greatly.
El Niño-Southern Oscillation
Ocean currents are in same direction as the wind – they become circular due to currents hitting land masses
ENSO El Nino / La Nina episodes of ocean warming and cooling
El Nino Southern Oscillation
El Niño is a large scale oceanographic / meteorological phenomenon that develops in the Pacific Ocean, which is associated with extreme climatic variability.
Short term Climate change
Ocean Currents
The 1997/98 ENSO event.
The 1997/98 ENSO event.
The 1997/98 ENSO event.
El Niño.
El Niño and La Niña.
Summary Global Circulation
NATS Lecture 15 Atmo-Ocean Interactions El Niño-Southern Oscillation
El Niño/La Niña.
Oceanic Circulation and ENSO
Presentation transcript:

Upwelling associated with ENSO events Colleen McHugh

Peruvian Upwelling Easterly trade winds Sea surface is higher and warmer near Indonesia (relative to Peru) Southerly winds off the coast of Peru  Ekman transport to the left of motionupwelling

Peruvian Upwelling

ENSO Easterly trade winds will weaken in Northern Hemisphere spring and occasionally reverse direction Ocean temperatures warm in central and eastern Pacific Thermocline flattens, preventing upwelling from occurring Has major oceanic and atmospheric impacts

How ENSO affects upwelling in Peru Thermocline deepens Nutrients from deeper waters don’t reach the surface Plankton and fish that rely on these nutrients will either die or migrate Major effects on fisheries and Peruvian economy

La Nina and upwelling Trade winds strengthen Leads to cooler waters and more upwelling

Resources http://earthobservatory.nasa.gov/Features/ElNino/elnino.php http://education.nationalgeographic.com/education/encyclopedia/el-nino/?ar_a=1 http://earthobservatory.nasa.gov/Features/LaNina/ http://ww2010.atmos.uiuc.edu/(Gl)/guides/mtr/eln/upw.rxml http://www.ncdc.noaa.gov/teleconnections/enso/enso-tech.php