Atlantic Meridional Transport Observed From Space Preliminry Results W. Timothy Liu and Xiaosu Xie  Heat Transport  Water Transport  Mean and Seasonal.

Slides:



Advertisements
Similar presentations
1 Dynamical Polar Warming Amplification and a New Climate Feedback Analysis Framework Ming Cai Florida State University Tallahassee, FL 32306
Advertisements

The ocean and the global hydrologic cycle Jim Carton (University of Maryland) Paulo Nobre (INPE) São Paulo Summer School on Global Climate Modeling October,
TROPICAL -- EXTRATROPICAL CONNECTIONS INCLUDING MARK A. CANE LAMONT-DOHERTY EARTH OBSERVATORY OF COLUMBIA UNIVERSITY PALISADES, NY PAUL GOODMAN.
Improving our understanding of the hydrological cycle and its changes: Observational and modelling needs Kevin E. Trenberth NCAR Improving our understanding.
RAPID/MOCHA/WBTS THE SEASONAL CYCLE OF THE AMOC AT 26ºN Eastern Boundary Considerations Gerard McCarthy, Eleanor Frajka- Williams, Aurélie Duchez and David.
Atmospheric Influences Physical oceanography Instructor: Dr. Cheng-Chien LiuCheng-Chien Liu Department of Earth Sciences National Cheng Kung University.
Can Amazon rainfall influence Winter Weather over Europe and North America and North Atlantic Oscillation? Rong Fu Robert Dickinson, Mingxuan Chen, Hui.
Preliminary results on Formation and variability of North Atlantic sea surface salinity maximum in a global GCM Tangdong Qu International Pacific Research.
Circulation in the atmosphere
The influence of extra-tropical, atmospheric zonal wave three on the regional variation of Antarctic sea ice Marilyn Raphael UCLA Department of Geography.
Ocean-atmosphere Coupling over Midlatitude Ocean Fronts 1. Difference between Wind & Stress 2. Signature above Boundary Layer W. Timothy Liu, Xiaosu Xie,
Class #16 Monday, October 4, 2010 Class #16: Monday, October 4 Chapter 8 Oceanography and El Niño/La Niña/ENSO 1.
What drives the oceanic circulation ? Thermohaline driven Wind driven.
1 Surface Circulation Pathways Generally, warm currents move poleward and cool currents move equatorward.
The Global Heat Budget Air-sea exchanges of heat (& freshwater) create deep water masses & drive the conveyor belt Heat source into the ocean is solar.
1 SOEE3410: Lecture 13 Ocean Mixed Layer. 2 What is the mixed layer? Why is it important? How do the atmosphere and ocean-surface interact? Example of.
5.7 PW5.9 PW The seasonal cycle of energy fluxes in the high latitudes Aaron Donohoe I.) How do the absorbed solar (ASR), outgoing longwave (OLR), and.
What drives the oceanic circulation ? Thermohaline driven (-> exercise) Wind driven (-> Sverdrup, Ekman)
Thermohaline Circulation
Advanced Oceanography Ocean Circulation - Chapter 1 A Review Circulation in both the oceans and the atmosphere is driven by energy from the Sun and modified.
Outline Background, climatology & variability Role of snow in the global climate system Indicators of climate change Future projections & implications.
` Inflow 14.1 Adapted from Gordon, 2005.
Observational evidence for propagation of decadal spiciness anomalies in the North Pacific Yoshi N. Sasaki, N. Schneider, N. Maximenko, and K. Lebedev.
© Imperial College LondonPage 1 Quantifying the direct radiative effect of Saharan dust aerosol over north-west Africa and the tropical Atlantic Richard.
=(S,,0); 4=(S,,4000).
Lecture 7: The Oceans (1) EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p
Potential temperature ( o C, Levitus 1994) Surface Global zonal mean.
Graduate Course: Advanced Remote Sensing Data Analysis and Application SURFACE HEAT BUDGETS IN THE PACIFIC WARM POOL DURING TOGA COARE Shu-Hsien Chou Dept.
Satellite Data Assimilation into a Suspended Particulate Matter Transport Model.
Oceanography 569 Oceanographic Data Analysis Laboratory Kathie Kelly Applied Physics Laboratory 515 Ben Hall IR Bldg class web site: faculty.washington.edu/kellyapl/classes/ocean569_.
Review of ocean temperature, salinity and oxygen changes in the Pacific and subtropical southern hemisphere Red = In IPCC AR4 Green = after IPCC AR4 Climate.
Are Tropical Cyclones Changing the Meridional Overturning Circulation? Gino.
Part II: Where are we going? Like an ocean... The waves crash down... Introducing OCEAN ATMOSPHERE INTERACTION.
Global Scale Energy Fluxes: Comparison of Observational Estimates and Model Simulations Aaron Donohoe -- MIT David Battisti -- UW CERES Science Team Meeting.
Variation of Surface Soil Moisture and its Implications Under Changing Climate Conditions 1.
Michael J. McPhaden, NOAA/PMEL Dongxiao Zhang, University of Washington and NOAA/PMEL Circulation Changes Linked to ENSO- like Pacific Decadal Variability.
Diagnostics, Special Projects and Phenomena of Interest Review of 2 nd C20C Workshop for 3 rd C20C Workshop ICTP, Trieste, Italy, 21 April 2004.
Sensitivity to precipitable water content and profile Resolution and Dynamical Core Dependence of the Statistics of Atmospheric River events in Community.
Long-Term Changes in Northern and Southern Annular Modes Part I: Observations Christopher L. Castro AT 750.
Kinematic Structure of the WAFR Monsoon ATS mb NCEP Climatology Zonal Winds.
TESTING THE REALISM OF THE MMF (or any GCM) REPRESENTATION OF THE MJO William B. Rossow Eric Tromeur City College of New York CMMAP Meeting July.
Aspen DCPP Workshop June 2015 Some critical technical choices for pacemaker experiments Christophe Cassou (Cerfacs-CNRS) Emilia Sanchez-Gomez (Cerfacs)
How Does Air Move Around the Globe?
An evaluation of satellite derived air-sea fluxes through use in ocean general circulation model Vijay K Agarwal, Rashmi Sharma, Neeraj Agarwal Meteorology.
Investigation of Mixed Layer Depth in the Southern Ocean by using a 1-D mixed layer model Chin-Ying Chien & Kevin Speer Geophysical Fluid Dynamics Institute,
Typical Distributions of Water Characteristics in the Oceans.
Prospects for Ocean (Re)analyses James A. Carton University of Maryland Benjamin S. Giese Texas A&M University Outline: Current analyses Global heat storage:
Ekman pumping Integrating the continuity equation through the layer:. Assume and let, we have is transport into or out of the bottom of the Ekman layer.
Graduate Course: Advanced Remote Sensing Data Analysis and Application Satellite-Based Tropical Warm Pool Surface Heat Budgets Shu-Hsien Chou Department.
Impact of wind-surface current covariability on the Tropical Instability Waves Tropical Atlantic Meeting Paris, France October 18, 2006 Tropical Atlantic.
Ocean Surface heat fluxes Lisan Yu and Robert Weller
Ocean Surface heat fluxes
Jim Angell’s contributions to understanding the QBO.
Contributions to SST Anomalies in the Atlantic Ocean [Ocean Control of Air-Sea Heat Fluxes] Kathie Kelly Suzanne Dickinson and LuAnne Thompson University.
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.
Wind-driven circulation II ●Wind pattern and oceanic gyres ●Sverdrup Relation ●Vorticity Equation.
FIGURE S5.1 Mean (1983–2004) shortwave radiation (W/m 2 ) from the International Satellite Cloud Climatology Project (ISCCP). (a) annual, (b) January,
Tropical Atlantic SST in coupled models; sensitivity to vertical mixing Wilco Hazeleger Rein Haarsma KNMI Oceanographic Research The Netherlands.
Michael J. McPhaden, NOAA/PMEL Dongxiao Zhang, University of Washington and NOAA/PMEL Circulation Changes Linked to ENSO- like Pacific Decadal Variability.
Dynamic Climatology Presentation Speaker : Pei-Yu Chueh Date : 2011/01/10.
LIMITLESS POTENTIAL | LIMITLESS OPPORTUNITIES | LIMITLESS IMPACT Copyright University of Reading AIR-SEA FLUXES FROM ATMOSPHERIC REANALYSES Richard Allan.
Our water planet and our water hemisphere
Energy constraints on Global Climate
A Comparison of Profiling Float and XBT Representations of Upper Layer Temperature Structure of the Northwestern Subtropical North Atlantic Robert L.
OCEAN RESPONSE TO AIR-SEA FLUXES Oceanic and atmospheric mixed
Intraseasonal latent heat flux based on satellite observations
Heat Transport by the Atmosphere and ocean
Oceanic Origin of the Precipitation Jump in the Sahel
New energy budget estimates at top of Earth’s atmosphere and surface
New energy budget estimates at top of Earth’s atmosphere and surface
Presentation transcript:

Atlantic Meridional Transport Observed From Space Preliminry Results W. Timothy Liu and Xiaosu Xie  Heat Transport  Water Transport  Mean and Seasonal Variation

Center of cyclonic currents Ekman water transport Ekman heat transport τ x : Zonal stress Te: Potential temp. of Ekman layer : Mean potential temp. of the water column Sato, Polito, & Liu, 2002: GRL, 29(17) Sprintall & Liu, 2005: Oceanography, 18(4)

Center of cyclonic currents Meridional Heat Transport (MHT) H: Heat content ζ: Horizontal heat flux SW: Short wave radiation LW: Long wave radiation LH: Latent heat SH: Sensible heat By Green’s theorem Conservation of heat

Center of cyclonic currents Meridional Water Transport (MWT) P: Precipitation E: Evaporation Ψ: Horizontal mass flux R: River discharge By Green’s theorem Conservation of water mass

Total MHT at Atlantic MHT from surface heat flux MHT from heat storage change (Statistic- al model)

Intensification of poleward Ekman water transport from 1998 in the tropics Pacific Ekman water transport Anomaly Total

Intensification of poleward Ekman heat transport from 1999 in the tropical Atlantic Ekman heat transport anomaly 12N-14N SSM/I QuikSCAT 5S-8S

Ekman water transport in the subtropical Atlantic is correlated with NAO

Atlantic total northward water transport Atlantic Ekman water transport Peak poleward transport in winter in the tropics

Intensification of poleward Ekman water transport from 1998 in the tropics Atlantic Ekman water transport Total Anomaly

Ekman water transport anomaly 12N-14N SSM/I QuikSCAT 5S-8S Intensification of poleward Ekman water transport from 1998 in the tropical Atlantic

Ekman water transport in the subtropical Atlantic is correlated with NAO

Summary  Spacebased data provide almost continuous spatial and temporal coverages for Ekman and total meridional transport for a decade  Reality checks are needed  What is the relation between surface Ekman transport in the total meridional transport need physical interpolation.

backup