Oceancurrent.imos.org.au David Griffin & Madeleine Cahill CSIRO Marine and Atmospheric Research.

Slides:



Advertisements
Similar presentations
Chapter 15 Section - 1.
Advertisements

Assessment of Cryosat sea level anomaly using HF radar and SST imagery David Griffin & Madeleine Cahill CSIRO Marine and Atmospheric Research.
Somali Current TYLER JANOSKI. First, let’s talk about the South-Asian Monsoon  Monsoon develops because of temperature differences between land and sea.
General questions: are there barriers for cross-breeding in the oceans? Implications for evolutionary study (e.g., species stability), ecology (e.g., local.
Building Bluelink David Griffin, Peter Oke, Andreas Schiller et al. March 2007 CSIRO Marine and Atmospheric Research.
Observing and Modelling the East Australian Current and its Eddies using IMOS data and Bluelink models David Griffin, Madeleine Cahill and Peter Oke CSIRO.
ROAM – IMOS comparisons David Griffin | Madeleine Cahill | Peter Oke Gary Carroll | Uwe Rosebrock CSIRO Marine and Atmospheric Research.
The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology Synergy of altimetry with other data and.
East Australian Current (the EAC). Where is it? EAC Properties Warm, deep, fast, nutrient poor water 100 km wide by 500km deep 30 million m 3 /s transport!
Fog/Foggy Weather. Overview Types of fog –Advection fog –Radiation fog –Upslope fog –Evaporation (mixing) fog –Steam fog Fog formation (1)by cooling…
Chapter 5: Other Major Current Systems
Coastal Upwelling Equatorward winds along a coastline lead to offshore Ekman transport Mass conservation requires these waters replaced by cold, denser.
Lesson 11: El Niño Southern Oscillation (ENSO) Physical Oceanography
Introducing an Integrated Marine Observing System for Australia (IMOS). Gary Meyers (IMOS Director) and John Middleton (SAIMOS)
IMOS OceanCurrent - bringing ocean observations to users David Griffin and Madeleine Cahill 27 May 2015 CSIRO MARINE AND ATMOSPHERIC RESEARCH.
North Carolina Coastal Lows Rick Neuherz Service Hydrologist NWS Wilmington NC.
Mesoscale Eddies in Indian Ocean Cdr Manoj Kumar Singh India.
Remote Sensing: Observing a BIG COUNTRY David Griffin & Edward King CSIRO Marine and Atmospheric Research.
Tuesday February 26, 2013 (Ocean Water Circulation)
Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.
Ocean forecasting and hindcasting the need for remote sensing Dr David Griffin | Dr Peter Oke CSIRO Marine and Atmospheric Research.
Modelling the Ocean Response to a Tropical Cyclone on Australia's Northwest Shelf Madeleine Cahill, CMAR Peter Craig, CMAR Mike Herzfeld - CMAR Lou Mason.
Use of Envisat RA2 sea level observations in the Bluelink ocean modelling system David Griffin, Peter Oke and Madeleine Cahill. CSIRO Marine and Atmospheric.
AIR MASSES A large body of air with uniform temperature and moisture characteristics. They acquire their characteristics in source regions, because they.
Ocean Currents and Climate Bell Ringer: Let’s Review! 1) Please take a copy of the currents flowchart and paste it into your IAN. 2) Use your brain, the.
Tuesday April 5, 2011 (The Gulf Stream; Importance of Surface Currents; Deep Ocean Circulation)
Leeuwin Current Eddies Altimetry, HF radar and SST imagery David Griffin & Madeleine Cahill CSIRO Marine and Atmospheric Research.
Observations of Storms off the West Coast in 2012 from Seafloor Data David Atkinson, UVic Dept. of Geography Steve Mihaly, ONC Dilumie Abeysirigunawardena,
Understanding Local Diurnal Winds
Building Bluelink David Griffin, Peter Oke, Andreas Schiller et al. March 2007 CSIRO Marine and Atmospheric Research.
Explaining the extraordinary: operational oceanography in Australia David Griffin Madeleine Cahill, Jim Mansbridge.
2015. equator Normally, trade winds converge at the equator and push warm water westward. In the eastern Pacific, cold water rises to the surface - upwelling.
Surface Currents Movement of water that flow in the upper part of the ocean’s surface.
Currents microsite.smithsonianmag.com -.
Currents and Climate Chapter 5 Lesson 2 Miss Cook February, 2012.
Introductory Physical Oceanography (MAR 555) - Fall 2009
 Abnormally high surface ocean temperatures off the coast of South America  Causes unusual weather patterns across the globe El Nino.
What causes the wind to blow?
Real-time oceanography and extreme events David Griffin, Madeleine Cahill and Jim Mansbridge. CSIRO Marine and Atmospheric Research.
CURRENTS. III. CURRENTS- move large amounts of water A. Deep Water Currents (density driven) why does the density of water change? cooling, evaporation,
Lecture 9: Air-Sea Interactions EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p ; Ch. 16, p ; Ch. 17, p
A frontal eddy intensively sampled at sea and overflown by SARAL David Griffin, Moninya Roughan, Shane Keating, Amandine Schaeffer, Iain Suthers CSIRO.
Oceans Surface Currents. What are surface currents? Surface currents are horizontal, streamline movements of water that occur at or near the surface of.
Ocean Currents. The water in the ocean is constantly moving The water in the ocean is constantly moving Broad bands of ocean water that flow in one direction.
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.
Boundary Currents - combine knowledge of global winds and Ekman flow - surface transport can be determined from wind direction/velocity - surface transport.
JAPAN EAST SEA CRUISE III “JES 3” JANUARY & FEBRUARY 2000.
Oceans.
Impact of a warm ocean eddy’s circulation on hurricane-induced sea surface cooling with implications for hurricane intensity Richard M. Yablonsky and Isaac.
Chapter 11 S5 Currents and Climate.
El Niño and La Niña.
Ocean Currents & Global Climates
Simulating the variability of Florida Current frontal eddies
NASA’s Ocean Color Online Visualization and Analysis System
Warm Water Currents & Climate Cold Water Currents & Climate
NASA’s Ocean Color Online Visualization and Analysis System
ENSO El Nino / La Nina episodes of ocean warming and cooling
Wind-Driven Cross-Shelf Transport on a Shelf with Curvature
Ocean Currents.
Oceans Surface Currents.
Time mean MSLP bias (mbar) in CCSM its atmospheric component (CAM/AMIP). CCSM4 MSLP bias is weaker than CCSM3 bias in the northern subtropical maxima.
Ocean Currents Some key questions: What causes the ocean currents?
Ocean Currents Streamlike movements of water that occur at or near the surface of the ocean are called surface currents. Surface currents are wind driven.
El Niño and La Niña.
Winds vs. Currents An Analysis of Wind Forcing
Ocean Currents Some key questions: What causes the ocean currents?
Upwelling Currents.
Oceans Surface Currents.
Presentation transcript:

Oceancurrent.imos.org.au David Griffin & Madeleine Cahill CSIRO Marine and Atmospheric Research

David Griffin 2 |

David Griffin 3 |

18 Jan 2013: EAC as a laminar jet. Cooler shore temperature south of Brisbane. David Griffin 4 |

Geostrophic upwelling along coast e.g. at Coffs David Griffin 5 |

EAC wrapping around an eddy off Sydney David Griffin 6 |

+11days: Much more cool water at shore. David Griffin 7 |

Strong upwelling-favourable wind on 28 Jan David Griffin 8 |

Sfc flow offshore (to SE) at CH70 ADCP on 29 Jan, then strong reversal to N by 2 Feb. Why? David Griffin 9 |

Cloudy, so SST no good. Radar seems to disagree with ADCPs David Griffin 10 |

SST better by 2 Feb. Radar and ADCP both show flow to N. David Griffin 11 |

5 Feb: 10km-dia eddy 20km south of ADCPs. David Griffin 12 |

Summary: EAC geostrophic uplift, so cold water on shelf Strong wind upwelled cold water to surface Two processes drive eddy formation: 1) cold anomaly naturally cyclonic, but NB only 10km diameter 2) vorticity transfer from EAC to eddy David Griffin 13 |

21 June 2013 news item: Ocean currents too strong for NSW lobster fishers David Griffin 14 |

Cyclonic eddy formed off Newcastle on 5/3/13. Argo: 200m upward heave off JB 16/4/13 David Griffin 15 |

Persistent northward flow on shelf JB-Syd for 6 weeks David Griffin 16 |

23 April 2013 David Griffin 17 |

16 May 2013 David Griffin 18 |

31 May 2013 David Griffin 19 |

16 June 2013 David Griffin 20 |

9 May 2013 glider track: 23 Mar-28 May David Griffin 21 |

Summary According to a lobster fisher’s 30-y diary, this year’s cyclonic eddy off JB was a very rare (long-lived) feature Sampled by an Argo float then a glider Replaced by a warm eddy, so Sydney’s coastal waters were ~2° warmer in May & June than April. David Griffin 22 |

Extreme current (and sea level) events in GAB David Griffin 23 |

SAIMOS ADCP data for David Griffin 24 |

David Griffin 25 |

21 May 2011 Pulse of flow to SE David Griffin 26 |

Westerly wind from small, deep low in GAB David Griffin 27 |

10 May 2012 David Griffin 28 |

8 May 2012 David Griffin 29 |

5 Sep 2012 David Griffin 30 |

4 Sep 2012 David Griffin 31 |

Summary Three cases similar, but do differ Why is the max current in inner shelf sometimes, and outer shelf other time? Need to investigate details of wind forcing; local vs propagating (CTW) components, and influence of eddies. David Griffin 32 |

Conclusions IMOS is producing a wealth of observations that are available to all, some in near-real time, others just a few mo afterwards. OceanCurrent provides a quick-look, to help everyone make best use of the data. News items draw attention to features of special interest. Please join the (too short!) list of contributors A special thanks to all our IMOS colleagues for doing the deployments and data management. David Griffin 33 |

David Griffin & Madeleine Cahill oceancurrent.imos.org.au CSIRO MARINE AND ATMOSPHERIC RESEARCH Thank you

David Griffin 35 |