Are Tropical Cyclones Changing the Meridional Overturning Circulation? Gino.

Slides:



Advertisements
Similar presentations
Global climate responses to perturbations in Antarctic Intermediate Water Jennifer Graham Prof K. Heywood, Prof. D. Stevens, Dr Z. Wang (BAS)
Advertisements

Analysis of Eastern Indian Ocean Cold and Warm Events: The air-sea interaction under the Indian monsoon background Qin Zhang RSIS, Climate Prediction Center,
Discussion 3/27 Midterm redux Lectures 14&15 Poster drafts.
The link between tropical convection and the Northern Hemisphere Arctic surface air temperature change on intraseaonal and interdecadal time scales Steven.
Better climate predictions using hindsight
Thermohaline circulation ●The concept of meridional overturning ●Deep water formation and property Antarctic Bottom Water North Atlantic Deep Water Antarctic.
Where Do the Hurricanes Come From?. Radiation Vapor/Cloud/precipitation Shallow convection Boundary layer turbulence Mesoscale convective system Thunderstorm.
Hurricanes and climate ATOC 4720 class22. Hurricanes Hurricanes intense rotational storm that develop in regions of very warm SST (typhoons in western.
Deep Tropical Convection contribution to climate change.
Clouds and Climate: Cloud Response to Climate Change SOEEI3410 Ken Carslaw Lecture 5 of a series of 5 on clouds and climate Properties and distribution.
Ocean Stratification and Circulation Martin Visbeck DEES, Lamont-Doherty Earth Observatory
Review - Precipitation is caused by the uplift of moist air Air rising along the ITCZ or weather fronts (convergence) Convection caused by intense surface.
Sea Surface Temperature, November Nomenclature Meridional Overturning Circulation (MOC): Total northward/southward flow, over latitude and.
Clouds and Climate: Cloud Response to Climate Change ENVI3410 : Lecture 11 Ken Carslaw Lecture 5 of a series of 5 on clouds and climate Properties and.
A monitoring design for the Atlantic meridional overturning circulation Joël Hirschi, Johanna Baehr, Jochem Marotzke, John Stark School of Earth and Ocean.
Thermohaline Circulation Carisa Sousa. Description Defining - terminology –Meridional Overturning Movement –“Overturning” - Pacific and Indian Oceans.
The Role of ENSO in Regulating its Background State De-Zheng Sun Tao Zhang CU/CIRES/Climate Diagnostics Center &NOAA/Earth System Research Laboratory Boulder,
Reconciling net TOA flux/ocean heating in observations and models 5-yr running means (Smith et al. 2015)Smith et al Spurious ocean data? CERES ERBS/reconReanalysis/recon.
5. Future climate predictions Global average temperature and sea-level are projected to rise under all IPCC scenarios Temperature: +1.8°C (B1) to +4.0°C.
Genesis Potential Index and ENSO Suzana J. Camargo.
© Oxford University Press, All rights reserved. 1 Chapter 6 CHAPTER 6 OCEAN–ATMOSPHERE INTERACTIONS.
Rotating Fluid -Part II A “GFD view” of the Ocean and the Atmosphere (a follow up Raymond’s Lectures) Arnaud Czaja.
The meridional coherence of the North Atlantic meridional overturning circulation Rory Bingham Proudman Oceanographic Laboratory Coauthors: Chris Hughes,
Walker Circulation. Mean Tropical Overturning Circulations (Figure obtained from Introduction to Tropical Meteorology, 2 nd Edition, © 2011 COMET.)
AOSC 200 Lesson 14. Oceanography The oceans plat three important roles in determining weather and climate (1) They are the major source of water vapor.
Effect of Tropical Biases on ENSO Simulation and Prediction Ed Schneider and Ben Kirtman George Mason University COLA.
Variability of Pacific Pycnocline Overturning in a Coupled GCM Bill Merryfield and George Boer Gu, D. and S.G.H. Philander, 1997: Inter- decadal climate.
Global Scale Energy Fluxes: Comparison of Observational Estimates and Model Simulations Aaron Donohoe -- MIT David Battisti -- UW CERES Science Team Meeting.
The Gent-McWilliams parameterization of ocean eddies in climate models Peter Gent National Center for Atmospheric Research.
The General Circulation of the Atmosphere and Oceans ATS 351 Lecture 9 November 2, 2009.
 In the mid-Pleistocene, the period of glacial cycles changed from 41kyr to 100kyr.  The zonal SST gradient increased during MPT due to the cooling in.
Three Lectures on Tropical Cyclones Kerry Emanuel Massachusetts Institute of Technology Spring School on Fluid Mechanics of Environmental Hazards.
Geothermal heating : the unsung diva of abyssal dynamics Julien Emile-Geay Lamont-Doherty Earth Observatory, Palisades, NY, USA Gurvan Madec LODYC, Paris,
Mean 20 o C isotherm (unit: meter) The thermocline zone is sometimes characterized by the depth at which the temperature gradient is a maximum (the “thermocline.
Role of the Gulf Stream and Kuroshio-Oyashio Systems in Large- Scale Atmosphere-Ocean Interaction: A Review Young-oh Kwon et al.
A Synthetic Drifter Analysis of Upper-Limb Meridional Overturning Circulation Interior Ocean Pathways in the Tropical/Subtropical Atlantic George Halliwell,
The General Circulation  The large-scale wind patterns of the earth  Mission: to mitigate global temperature contrasts (decrease temperature gradients,
Current state of ECHAM5/NEMO coupled model Wonsun Park, Noel Keenlyside, Mojib Latif (IFM-GEOMAR) René Redler (NEC C&C Research Laboratories) DRAKKAR meeting.
The CHIME coupled climate model Alex Megann, SOC 26 January 2005 (with Adrian New, Bablu Sinha, SOC; Shan Sun, NASA GISS; Rainer Bleck, LANL)  Introduction.
Ocean Climate Simulations with Uncoupled HYCOM and Fully Coupled CCSM3/HYCOM Jianjun Yin and Eric Chassignet Center for Ocean-Atmospheric Prediction Studies.
Latitudinal Gradients in the Earth’s Energy Budget.
Surface Energy Balance (1). Review of last lecture The mission of meteorology is to understand and predict weather- and climate-related disasters (e.g.
Benjamin A. Schenkel University at Albany, State University of New York, and Robert E. Hart, The Florida State University 4 th.
Multidecadal simulations of the Indian monsoon in SPEEDY- AGCM and in a coupled model Annalisa Bracco, Fred Kucharski and Franco Molteni The Abdus Salam.
Interannual to decadal variability of circulation in the northern Japan/East Sea, Dmitry Stepanov 1, Victoriia Stepanova 1 and Anatoly Gusev.
Lecture 12 Rossby waves, propagation, breaking, climatic effects
Atmospheric and Oceanic General Circulation Dr. John Krasting NOAA/GFDL – Princeton, NJ Rutgers Physical Climatology October 18,
EVAT 554 OCEAN-ATMOSPHERE DYNAMICS UPWELING AND DOWNWELLING; EKMAN TRANSPORT LECTURE 14 (Reference: Peixoto & Oort, Chapter 8,10)
Atlantic Meridional Transport Observed From Space Preliminry Results W. Timothy Liu and Xiaosu Xie  Heat Transport  Water Transport  Mean and Seasonal.
OCEAN CIRCULATION. DENSITY OF SEAWATER DENSITY INCREASES DEPTH INCREASES TEMP DECREASES SALINITY INCREASES EFFECT OF TEMP > EFFECT OF SALINITY.
Tropical Atlantic SST in coupled models; sensitivity to vertical mixing Wilco Hazeleger Rein Haarsma KNMI Oceanographic Research The Netherlands.
Judy Twedt ~ Kelly McCusker ~ Cecilia Bitz June 5, 2012 Judy Twedt ~ Kelly McCusker ~ Cecilia Bitz June 5, 2012 Effects of GeoEngineering on the Southern.
How ENSO influence the Luzon Strait transport 汇报人:叶瑞杰 专业年级: 2016 级物理海洋博士.
Tropical dynamics and Tropical cyclones
Our water planet and our water hemisphere
Jake Langmead-Jones The Role of Ocean Circulation in Climate Simulations, Freshwater Hosing and Hysteresis Jake Langmead-Jones.
Ocean Circulation.
Western Boundary Currents
The Atmosphere: Part 9: Short term climate variability
Global Changes in Climate
Walker Circulation.
Ocean circulation: key questions
Annual mean precipitation (colour), SST (contours) & surface wind
Relationship between ENSO and SST variation
Case Studies in Decadal Climate Predictability
Summary Global Circulation
NATS Lecture 15 Atmo-Ocean Interactions El Niño-Southern Oscillation
Oceans and Internal Climate Variability
Ocean Currents.
Surface Wave Enhanced Turbulence as an important source energy maintaining/regulating Thermohaline Circulation Rui Xin Huang Woods Hole Oceanographic.
Presentation transcript:

Are Tropical Cyclones Changing the Meridional Overturning Circulation? Gino

Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

OCEAN GHG Warming Wind Stress Increase MORE MIXING z EQ NS Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

Meridional TOA Net Radiation Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

2 Mechanism for MOC Isopycnal Diapynal Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

Net heating at this stage Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

Net Mixed Layer Cooling Price 1981 Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

Mixed at base of Mixed Layer Rightward bias Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

Ekman Pumping Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

- SSH: Ekman Pumping Cooling + SSH: Rightward Net Warming Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

Heat Content Calculation Net Cooling (Mixed Layer) Net Warming (Total Column) Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

Result Net Warming by TC : (Emanuel 01) Peak Poleward transport : (Macdonald and Wunsch 96) Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

MOC required mixing (Munk and Wunsch 98) ? TC induced MOC (Emanuel 01) ? Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

TC-mixed-parcel Track EQ 20N EQ Undercurrent PACIFIC OCEAN TC Mixing Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

No TC mixing Full Band TC mixing Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

Increase CO2 Only Increase CO2 Increase Vertical Diffusivity 8 – 40 N & S Increase CO2 Increase Vertical Diffusivity 8 – 40 N & S Preindustrial CO2 Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

Uvic Model (OGCM) Based on Modular Ocean Model Initialized with Modern Climatology No Dynamic Atmosphere 3000 yr Control Run: without TC mixing Exp Run: TC mixing parameterization Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

Subtropical Overturning Circulation dominates in 10N – 30N upper ocean TC Mixing effect confined in tropics! Heat Pump for MOC? Heat Pump for El Nino? MOC changed by TC?

reference Emanuel 2001 Contribution of tropical cyclones to meridional heat transport by the oceans Emanuel 2001 Fedorov 2009 Tropical cyclones and permanent El Niño in the early Pliocene epoch Fedorov 2009 Sriver 2010 Climate response to tropical cyclone-induced ocean mixing in an Earth system model of intermediate complexity Sriver 2010