El Nino Upwelling and Ocean Productivity

Slides:



Advertisements
Similar presentations
Upwelling in the World Ocean
Advertisements

Estimate the latitude where warm El Niño water is located.
El Niño & La Niña.
El Niño. How do ocean currents affect weather and climate? Oceans store and transport heat. – High heat capacity – Stores and transports energy from the.
Large-scale Satellite Oceanography in Eastern Pacific Upwelling Regions Andrew Thomas University of Maine Recent manuscript collaborators: Jose Luis Blanco,
1. During normal conditions, a ______ pressure zone forms over Indonesia, causing wind to blow _____________. A.High; Peru to Indonesia B.High; Indonesia.
Vertical temperature change ● Temperature – there are 3 temperature zones in the ocean. ● Surface to 200 meters – warmed by the Sun. ● Thermocline: 200.
El Niño Southern Oscillation [ENSO] NORMAL: - Easterly trade winds between ± 30° latitude (Coriolis Force) - Sea Surface Height slant to west - Warm basin.
Mean annual SST. EQ WestEast Equatorial Divergence.
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.
The 1997/98 ENSO event. Multivariate ENSO Index Index is based on 6 parameters relevant to phase.
El Nino – Southern Oscillation - Southern Oscillation (atmosphere) - El Nino (ocean) - change in equatorial Pacific circulation - produces global climate.
Bryson McNulty EAS-4480 Georgia Inst. Of Technology April 22 nd, 2014.
The Correlation between Atlantic Hurricane Frequency and ENSO Jessica Johnson EAS 4480 Spring 2012.
What weather phenomena has the largest impact on our weather in Texas?
Upwelling. What is upwelling? Upwelling video clip.
Do Now; Are there weather patterns that influence places thousands of miles away?
Assessing Predictability of Seasonal Precipitation for May-June-July in Kazakhstan Tony Barnston, IRI, New York, US.
El Nino and the Southern Oscillation Jon Schrage.
Oceanography Ocean Currents Chapter 24.1 and 24.2.
U. Victoria Regional Oceanography Affecting the NEPTUNE Array Ken Denman School of Earth and Ocean Sciences & Ocean Networks Canada University of Victoria,
Coastal Processes and El Nino. El Nino  Normal: Trade winds blow west Wind piles up warm water in W. Pacific ○ Sea surface and sea surface temperature.
Climate Change El-Nino Southern Oscillation (ENSO)Phenomena.
NATS Lecture 15 Atmo-Ocean Interactions El Niño-Southern Oscillation.
El Niňo. El Nińo: A significant increase in sea surface temperature over the eastern and central equatorial Pacific that occurs at irregular intervals,
1 Kelvin Waves El Niño October Ocean’s response to changing winds Ocean’s response to changing winds external (or surface)waves external (or surface)waves.
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.
Bailey Wright.  Tornadoes are formed when the vertical wind shear, vertical vorticity, and stream line vorticity conditions are favorable. ◦ Storms and.
1 What happened in 1982 El Nino? Mehmet ILICAK RSMAS, University of Miami 2005.
Currents & Climate Ch Warm-water currents i.e. Gulf Stream Creates mild climate at high latitudes such as British Isles (much warmer than Newfoundland.
Dr. Neil S. Suits. NASA/Goddard Space Flight Center, The SeaWiFS Project and GeoEye, Scientific Visualization Studio SeaWiFS Ocean Biosphere: 1997 to.
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.
Global Winds and Ocean Currents Ocean Currents are created by global winds. Ocean Currents are created by global winds. Global winds are created by the.
Exploring the Relationship Between North Atlantic and Global Temperature Anomalies Using Bivariate and Time Series Analysis EAS 4480 Ryan Schilling.
Climate Phenomena.
Upwelling in the World Ocean
El Niño and La Niña.
Upwelling in the World Ocean
Mentor: Dr. Jinchun Yuan
Ocean Currents & Global Climates
Ocean Circulation.
Please grab the “Dissolved Nutrients” reading passage.
Time scales of physics vs. biology
El Nino Southern Oscillation
16.1 – Ocean Circulation.
El Niño / Southern Oscillation (ENSO)
What weather phenomena has the largest impact on our weather in Texas?
El Nino and La Nina.
EL NINO Figure (a) Average sea surface temperature departures from normal as measured by satellite. During El Niño conditions upwelling is greatly.
Major ocean current systems
El Nino Southern Oscillation
Tree Rings vs. Annual Precipitation
David Tedesco Physical Oceanography
The 1997/98 ENSO event.
El Niño-Southern Oscillation
The 1997/98 ENSO event.
Upwelling in the World Ocean
The 1997/98 ENSO event.
Time scales of physics vs. biology
M1/M2 BUOY DATA: OCEAN TEMPERATURE ANALYSIS
El Niño and La Niña.
Aquatic Science Fall Final Review
Is global warming deoxygenating the ocean?
El Niño and the Southern Oscillation (“ENSO”)
NATS Lecture 15 Atmo-Ocean Interactions El Niño-Southern Oscillation
Upwelling Currents.
Wind Wind is created by solar energy. More specifically wind is created by the uneven heating of the Earth. Reasons why the Earth heats unevenly: 1)
Presentation transcript:

El Nino Upwelling and Ocean Productivity By Sonia Muhammad

Motivation Show that upwelling during El Nino affects the ocean productivity on the coasts of Southern Peru/Northern Chile and Southern California

Upwelling Sea Surface Temperature Sea Surface Height Anomaly During El Nino, warm current appears on the coast, and upwelling diminishes Sea Surface Height Anomaly We can determine if upwelling is diminished by observing the sea surface height, which tells us if a warm current is present. (Depression of thermocline leads to a higher SSH) Warm Current Upwelling Diminishes Less Nutrients at Surface Productivity Decreases Warm Current Displaces Colder Water in Upper Layer Sea Surface Height Increases Elevation of Thermocline Upwelling Diminished Productivity Decreases

Data HadISST for Sea Surface Temperature AVISO for Sea Surface Height Anomaly SeaWiFS for Chlorophyll Concentration Chlorophyll concentration data can be used to observe ocean productivity aka amount of phytoplankton

Least Squares Regression Analysis

Peru: SST vs Chlorophyll

Peru: SST vs Chlorophyll Correlation Coefficient LS Slope Value -0.07 -0.0061 95 % Confidence Interval -0.23 to 0.09 -0.18 to 0.17 Significance 0.38 Very weak negative correlation and small confidence interval, however the correlation value has little significance as the p value is much greater than 5 %.

Peru: SSH vs Chlorophyll

Peru: SSH vs Chlorophyll Correlation Coefficient LS Slope Value -0.10 -0.1968 95 % Confidence Interval -0.25 to 0.06 -4.24 to 3.85 Significance 0.24 Weak negative correlation, small confidence interval, however the correlation value has little significance as the p value is much greater than 5 %.

SoCal: Chlorophyll vs SST

SoCal: Chlorophyll vs SST Correlation Coefficient LS Slope Value -0.33 -0.07 95 % Confidence Interval -0.46 to -0.18 -0.47 to 0.33 Significance 0.00002 Weak negative correlation and small confidence interval, and the correlation value has high significance as the p value is much less than 5 %.

SoCal: Chlorophyll vs SSH

SoCal: Chlorophyll vs SSH Correlation Coefficient LS Slope Value 0.40 4.3554 95 % Confidence Interval -0.26 to 0.52 -15.50 to 24.22 Significance 3.04 e-7 Weak positive correlation, small confidence interval for the correlation coefficient, and the correlation value has very high significance as the p value is much greater than 5 %. As for the LS slope, the confidence interval is very large, and shows a large positive slope.

Peru: Periodicity

SoCal: Periodicity

Peru: Cross Spectral Analysis (SSH) f = .0795 Period =12.5833 months Lag = 0.1221 Δt = 0.0017 years = .20 months = .6 days

SoCal: Cross Spectral Analysis (SSH) f = .0779 Period =12.833 Lag = 0.5467 Δt = 0.0076 years = .09 months = 2.7 days

Peru: Cross Spectral Analysis (SST) f = .0795 Period =12.583 Lag = .1588 Δt = 0.0022 years = .0264 months = .8days

SoCal: Cross Spectral Analysis (SST) f = .0779 Period =12.833 Lag = 0.6605 Δt = 0.0092 years = .11 months = 3 days