Global sea surface temperature October 25 th 2007

Size: px
Start display at page:

Download "Global sea surface temperature October 25 th 2007"

Transcription

1 The VOCALS Regional Experiment Aerosols, clouds, and precipitation in southeast Pacific stratocumulus Robert Wood Atmospheric Sciences University of Washington

2 Global sea surface temperature October 25 th

3 ISCCP inferred St/Sc amount

4 Twomey Albrecht

5 Rich marine habitats, few continental ones SeaWIFS Ocean Color Tarapacá, Atacama Desert Net primary productivity of Humboldt current 3 tc ha 1 yr 1 Net primary productivity of boreal forests 2 8 tc ha 1 yr 1 Iquique annual precipitation nfall [mm] rain

6 20 o S

7 Longitudinal cross section at 20 o S 85 o W 65 o W

8

9 SST anomaly from zonal mean ERBE net cloud ERBE net cloud forcing

10 A coupled problem Correct prediction of stratus properties is important for the correct prediction of the climate over the tropical warm pool connections with ITCZ through both ocean and atmosphere Yu and Mechoso 2001 Precip [mm day 1 ]

11 SST Biases in Coupled Models SST Biases in NCAR CCSM (Collins et al. 2006)

12 Ocean surface heat budget Net heat input into ocean at center of stratus sheet > 50 W m 2 2 Must be corresponding cold water transport from somewhere Annual Heat Fluxes 20 o S, 85 o W 250 Net SW W W/m Net LW Latent Sensible Net Heat Bob Weller, WHOI

13 Mesoscale ocean eddies Mesoscale ocean eddies form in coastal upwelling regions and propagate westward Their impact on the heat, nutrient, and freshwater budgets is poorly known They are not resolved in coupled GCMS Simulation from Penven et al. (2005)

14 Mesoscale ocean eddies Height SST Eddies impact SST and can be observed using altimetry courtesy Shang Ping Xie, University of Hawaii

15

16 14 year animation of eddies identified using satellite altimetry (courtesy Dudley Chelton, OSU)

17 Clouds and cloud processes

18 ERBE SWCF (W m 2 ) NCAR GFDL Clouds in Global l Models GMAO Annual mean Control run Atmospheric models

19 Why this Uncertainty? resolution of ~5m required to resolve inversion! ~12K! Free tropospheric T set by ITCZ θ e 2,000km ~1km BL T set by local SST

20 Drizzle is important over the SEP

21 Mesoscale variability in stratocumulus

22 200 km Pockets of Open Cells (POCs)

23 Mesoscale stratocumulus structure Cloud albedo strongly gy dependent upon open/closed cells Open Cells Low albedo Satellite Closed Cells 100 km Strong precipitation associated with open cell structure High albedo Open cells form in clear marine environment potential anthropogenic impacts Strong drizzle Ship Radar Weak drizzle

24 Drizzle and cloud droplet concentration EPIC data, Bretherton et al. (2004)

25 POCs and Aerosols Strong reductions in accumulation mode aerosol concentration New nucleation Links between aerosol microphysics i and cloud macrophysics?

26 Global cloud droplet concentration (MODIS, annual mean ) 2004)

27 Cloud Microphysical i Variability Smelter locations MODIS Cloud Droplet Concentration (SON ) Cloud droplet concentration [cm 3 ]

28 The VAMOS Ocean-Cloud-Atmosphere- Land Study Ai t t ti iti l di t i d d t di d d l Aim: to promote activities leading to improved understanding and model predictions of the SEP coupled system on diurnal to interannual timescales

29

30 THE VOCALS STRATEGY

31 VOCALS Regional Experiment (REx) VOCALS Rex will collect datasets required to address a set of issues that are organized into two broad themes: Aerosol cloud drizzle interactions in the marine boundary layer (MBL) and the physicochemical and spatiotemporal properties of aerosols Chemical and physical couplings between the upper ocean, the land, and the atmosphere.

32 VOCALS REx Platforms NSF C 130 NOAA Ronald ldh Brown DoE ASP G 1 CIRPAS Twin Otter

33 The aircraft DoEASP G 1 CIRPAS Twin Otter Chemistry and aerosols, cloud microphysics, turbulence Remote sensing and cloud imaging NERC Dornier 228 NSF C 130 Chemistry and aerosols, cloud microphysics, turbulence, radar/lidar remote sensing Radar remote sensing, microphysics, turbulence Aerosols, cloud microphysics, i radiative measurements UK FAAM BAe 146

34 The Ships IMARPE José Olaya NOAA Ronald H Brown

35 VOCALS REx Platforms and Sampling Aircraft: NSF C 130 CIRPAS Twin Otter DoE G 1 UK BAe 146 NERC Do 228 Ships: NOAA Ronald H Brown José Olaya Land sites: Iquique Paposo

36 VOCALS-REx Cross-Section Sampling Combined NOAA Ronald H Brown and NSF C 130 Missionsi direct evaluation of GCM lower direct evaluation of GCM lower tropospheric structure

37 Flight plan for C 130 POC Drift missions

38

39 Operations Bases Arica (Operations Center) C 130, G 1, UK 146, Do228 Iquique CIRPAS Twin Otter, Sounding station Paposo Ground station for aerosol characterization

40

Oceanic Eddies in the VOCALS Region of the Southeast Pacific Ocean

Oceanic Eddies in the VOCALS Region of the Southeast Pacific Ocean Oceanic Eddies in the VOCALS Region of the Southeast Pacific Ocean Outline: Overview of VOCALS Dudley B. Chelton Oregon State University Overview of the oceanographic component of VOCALS Preliminary analysis

More information

Atmosphere-Ocean-Land Interaction Theme. VOCALS Preparatory Workshop - NCAR, May 18-29, 2007

Atmosphere-Ocean-Land Interaction Theme. VOCALS Preparatory Workshop - NCAR, May 18-29, 2007 Atmosphere-Ocean-Land Interaction Theme VOCALS Preparatory Workshop - NCAR, May 18-29, 2007 The Southeastern Pacific Cloud-topped ABLs, with mesoscale structures Influenced by and influential on remote

More information

A review of VOCALS Hypothesis. VOCALS Science Meeting July 2009 Seattle Washington C. R. Mechoso, UCLA

A review of VOCALS Hypothesis. VOCALS Science Meeting July 2009 Seattle Washington C. R. Mechoso, UCLA A review of VOCALS Hypothesis VOCALS Science Meeting 12-14 July 2009 Seattle Washington C. R. Mechoso, UCLA VOCALS Strategy MODELING Operational Centers, Reseach Institutions, Universities REx AIRBORNE

More information

VOCALS Cloud-Drizzle-Aerosol Theme

VOCALS Cloud-Drizzle-Aerosol Theme VOCALS Cloud-Drizzle-Aerosol Theme Understanding and modeling aerosol indirect effects Is drizzle important to Sc synoptic variability and climatology? IPCC, 2007 AEROSOL-CLOUD-PRECIPITATION HYPOTHESES

More information

A synthesis of published VOCALS studies on marine boundary layer and cloud structure along 20S

A synthesis of published VOCALS studies on marine boundary layer and cloud structure along 20S A synthesis of published VOCALS studies on marine boundary layer and cloud structure along 20S Chris Bretherton Department of Atmospheric Sciences University of Washington VOCALS RF05, 72W 20S Work summarized

More information

It is possible that it does, although most steps are too poorly quantified to be certain. CLAW Hypothesis

It is possible that it does, although most steps are too poorly quantified to be certain. CLAW Hypothesis The CLAW Hypothesis Does anyone believe that this feedback loop works as advertised? It is possible that it does, although most steps are too poorly quantified to be certain. CLAW Hypothesis Charlson,

More information

1. The Southeast Pacific Climate System

1. The Southeast Pacific Climate System VOCALS The VAMOS Ocean-Cloud-Atmosphere-Land Study Improving understanding, model simulations, and prediction of the Southeast Pacific Climate System PROGRAM SUMMARY June 2007 Robert Wood, VOCALS-REx PI,

More information

Warm rain and climate: VOCALS, CloudSat, Models. Robert Wood University of Washington

Warm rain and climate: VOCALS, CloudSat, Models. Robert Wood University of Washington Warm rain and climate: VOCALS, CloudSat, Models Robert Wood University of Washington Warm rain a missing climatology Image: NASA GSFC Shipboard remote sensing shows frequent precipitation from shallow

More information

Part 3 Selected Modeling and Preliminary Confrontation with VOCALS Hypothesis

Part 3 Selected Modeling and Preliminary Confrontation with VOCALS Hypothesis Part 3 Selected Modeling and Preliminary Confrontation with VOCALS Hypothesis Transition to deep convection Shallow convection Transition to shallow convection Coastal clearing Aerosol VOCALS Paradigm

More information

NSF 2005 CPT Report. Jeffrey T. Kiehl & Cecile Hannay

NSF 2005 CPT Report. Jeffrey T. Kiehl & Cecile Hannay NSF 2005 CPT Report Jeffrey T. Kiehl & Cecile Hannay Introduction: The focus of our research is on the role of low tropical clouds in affecting climate sensitivity. Comparison of climate simulations between

More information

How is precipitation from low clouds important for climate?

How is precipitation from low clouds important for climate? How is precipitation from low clouds important for climate? CloudSat estimated precipitation rate from low clouds Low clouds over the SE Pacific, Nov 11 th 2014 Robert Wood, University of Washington With

More information

Warm rain variability and its association with cloud mesoscalestructure t and cloudiness transitions. Photo: Mingxi Zhang

Warm rain variability and its association with cloud mesoscalestructure t and cloudiness transitions. Photo: Mingxi Zhang Warm rain variability and its association with cloud mesoscalestructure t and cloudiness transitions Robert Wood, Universityof Washington with help and data from Louise Leahy (UW), Matt Lebsock (JPL),

More information

Surface flux observations on the southeastern tropical Pacific Ocean and attribution. of SST errors in coupled ocean-atmosphere models

Surface flux observations on the southeastern tropical Pacific Ocean and attribution. of SST errors in coupled ocean-atmosphere models Surface flux observations on the southeastern tropical Pacific Ocean and attribution of SST errors in coupled ocean-atmosphere models SIMON P. DE SZOEKE * Oregon State University College of Ocean and Atmospheric

More information

Ship observations coasting South America. in the tropical Pacific Ocean

Ship observations coasting South America. in the tropical Pacific Ocean Ship observations coasting South America in the tropical Pacific Ocean S. P. de Szoeke, C. W. Fairall, and Sergio Pezoa NOAA/ESRL Physical Sciences Division, Boulder, Colorado, USA. NOAA/ESRL/Physical

More information

EVIDENCE FOR NATURAL VARIABILITY IN MARINE STRATOCUMULUS CLOUD PROPERTIES DUE TO CLOUD-AEROSOL INTERACTIONS

EVIDENCE FOR NATURAL VARIABILITY IN MARINE STRATOCUMULUS CLOUD PROPERTIES DUE TO CLOUD-AEROSOL INTERACTIONS EVIDENCE FOR NATURAL VARIABILITY IN MARINE STRATOCUMULUS CLOUD PROPERTIES DUE TO CLOUD-AEROSOL INTERACTIONS Bruce Albrecht 1, Tarah Sharon 1, Haf Jonsson 2, Patrick Minnis 3, J. Kirk Ayers 4, Mandana M.

More information

Measurements are infrequent in this region due to difficulty in making both ship- and air-based measurements Natural pristine region far removed from

Measurements are infrequent in this region due to difficulty in making both ship- and air-based measurements Natural pristine region far removed from PLANNED OBSERVATIONAL CAMPAIGNS OVER THE SOUTHERN OCEANS FOR DETERMINING THE ROLES OF CLOUDS, AEROSOLS AND RADIATION IN THE CLIMATE SYSTEM: SOCRATES, MARCUS & MICRE G. McFarquhar, U. Illinois C. Bretherton,

More information

Differences from CERES EBAF

Differences from CERES EBAF Summary of Session 3 (16 talks) A. Protat, S. Siems, R. Marchand Talk 1: Kalli Furtado (UKMO) SO SST bias linked to lack of SLW clouds in the UM model Developed a new parameterization using turbulence

More information

On Surface fluxes and Clouds/Precipitation in the Tropical Eastern Atlantic

On Surface fluxes and Clouds/Precipitation in the Tropical Eastern Atlantic On Surface fluxes and Clouds/Precipitation in the Tropical Eastern Atlantic Chris Fairall, NOAA/ESRL Paquita Zuidema, RSMAS/U Miami with contributions from Peter Minnett & Erica Key AMMA Team Meeting Leeds,

More information

Comparison of Convection Characteristics at the Tropical Western Pacific Darwin Site Between Observation and Global Climate Models Simulations

Comparison of Convection Characteristics at the Tropical Western Pacific Darwin Site Between Observation and Global Climate Models Simulations Comparison of Convection Characteristics at the Tropical Western Pacific Darwin Site Between Observation and Global Climate Models Simulations G.J. Zhang Center for Atmospheric Sciences Scripps Institution

More information

EPIC2001 was conceived as an intensive process study along and near 95 o W during September and October 2001 used to make measurements of the atmosphe

EPIC2001 was conceived as an intensive process study along and near 95 o W during September and October 2001 used to make measurements of the atmosphe EPIC2001 was conceived as an intensive process study along and near 95 o W during September and October 2001 used to make measurements of the atmosphere and ocean in this region. Two aircraft, the National

More information

Boundary layer parameterization and climate. Chris Bretherton. University of Washington

Boundary layer parameterization and climate. Chris Bretherton. University of Washington Boundary layer parameterization and climate Chris Bretherton University of Washington Some PBL-related climate modeling issues PBL cloud feedbacks on tropical circulations, climate sensitivity and aerosol

More information

Influence of Clouds and Aerosols on the Earth s Radiation Budget Using Clouds and the Earth s Radiant Energy System (CERES) Measurements

Influence of Clouds and Aerosols on the Earth s Radiation Budget Using Clouds and the Earth s Radiant Energy System (CERES) Measurements Influence of Clouds and Aerosols on the Earth s Radiation Budget Using Clouds and the Earth s Radiant Energy System (CERES) Measurements Norman G. Loeb Hampton University/NASA Langley Research Center Bruce

More information

VOCALS REx: Aerosol Physics at the Ocean Surface On the NOAA RV Ronald H. Brown October, November 2008

VOCALS REx: Aerosol Physics at the Ocean Surface On the NOAA RV Ronald H. Brown October, November 2008 VOCALS REx: Aerosol Physics at the Ocean Surface On the NOAA RV Ronald H. Brown October, November 8 Catherine Hoyle, NOAA PMEL Derek Coffman, NOAA PMEL Tim Bates, NOAA PMEL Trish Quinn, NOAA PMEL Lelia

More information

VAMOS Ocean-Cloud-Atmosphere-Land Study (VOCALS) Science Plan. Draft: January 18, Prepared by the VOCALS Scientific Working Group

VAMOS Ocean-Cloud-Atmosphere-Land Study (VOCALS) Science Plan. Draft: January 18, Prepared by the VOCALS Scientific Working Group VAMOS Ocean-Cloud-Atmosphere-Land Study (VOCALS) Science Plan Draft: January 18, 2005 Prepared by the VOCALS Scientific Working Group 1 1. Introduction to VOCALS Interactions between the South American

More information

How surface latent heat flux is related to lower-tropospheric stability in southern subtropical marine stratus and stratocumulus regions

How surface latent heat flux is related to lower-tropospheric stability in southern subtropical marine stratus and stratocumulus regions Cent. Eur. J. Geosci. 1(3) 2009 368-375 DOI: 10.2478/v10085-009-0028-1 Central European Journal of Geosciences How surface latent heat flux is related to lower-tropospheric stability in southern subtropical

More information

An Introduction to Climate Modeling

An Introduction to Climate Modeling An Introduction to Climate Modeling A. Gettelman & J. J. Hack National Center for Atmospheric Research Boulder, Colorado USA Outline What is Climate & why do we care Hierarchy of atmospheric modeling strategies

More information

Upsidence wave during VOCALS. David A. Rahn and René Garreaud Department of Geophysics Universidad de Chile

Upsidence wave during VOCALS. David A. Rahn and René Garreaud Department of Geophysics Universidad de Chile Upsidence wave during VOCALS David A. Rahn and René Garreaud Department of Geophysics Universidad de Chile Upsidence Wave Garreaud and Muñoz (2004, GM04) A robust diurnal cycle of vertical motion between

More information

Clouds in the Climate System: Why is this such a difficult problem, and where do we go from here?

Clouds in the Climate System: Why is this such a difficult problem, and where do we go from here? Clouds in the Climate System: Why is this such a difficult problem, and where do we go from here? Joel Norris Scripps Institution of Oceanography CERES Science Team Meeting April 29, 2009 Collaborators

More information

Upsidence wave during VOCALS. David A. Rahn and René Garreaud Department of Geophysics Universidad de Chile

Upsidence wave during VOCALS. David A. Rahn and René Garreaud Department of Geophysics Universidad de Chile Upsidence wave during VOCALS David A. Rahn and René Garreaud Department of Geophysics Universidad de Chile Upsidence Wave Garreaud and Muñoz (2004, GM04) A robust diurnal cycle of vertical motion between

More information

How Will Low Clouds Respond to Global Warming?

How Will Low Clouds Respond to Global Warming? How Will Low Clouds Respond to Global Warming? By Axel Lauer & Kevin Hamilton CCSM3 UKMO HadCM3 UKMO HadGEM1 iram 2 ECHAM5/MPI OM 3 MIROC3.2(hires) 25 IPSL CM4 5 INM CM3. 4 FGOALS g1. 7 GISS ER 6 GISS

More information

Preliminary Observations

Preliminary Observations Aerosol Physiochemical Properties and Dynamics during VOCALS: Advection, Removal and Entrainment VOCALS Workshop July 12-14, 2009 A. Clarke, S. Howell, C. McNaughton, V. Kapustin, S. Freitag, L. Shank,

More information

The Atmospheric Boundary Layer. The Surface Energy Balance (9.2)

The Atmospheric Boundary Layer. The Surface Energy Balance (9.2) The Atmospheric Boundary Layer Turbulence (9.1) The Surface Energy Balance (9.2) Vertical Structure (9.3) Evolution (9.4) Special Effects (9.5) The Boundary Layer in Context (9.6) What processes control

More information

Ultra clean layers and low albedo ( grey ) clouds in CSET

Ultra clean layers and low albedo ( grey ) clouds in CSET CSET RF11, near Hawaii Ultra clean layers and low albedo ( grey ) clouds in CSET Robert Wood, University of Washington Paquita Zuidema, Chris Bretherton, Kuan Ting (Andy) O, Hans Mohrmann, Isabel McCoy,

More information

Evaluation of stratocumulus cloud prediction in the Met Office forecast model during VOCALS-REx

Evaluation of stratocumulus cloud prediction in the Met Office forecast model during VOCALS-REx Atmos. Chem. Phys., 10, 10541 10559, 2010 doi:10.5194/acp-10-10541-2010 Author(s) 2010. CC Attribution 3.0 License. Atmospheric Chemistry and Physics Evaluation of stratocumulus cloud prediction in the

More information

Large-Eddy Simulations of Tropical Convective Systems, the Boundary Layer, and Upper Ocean Coupling

Large-Eddy Simulations of Tropical Convective Systems, the Boundary Layer, and Upper Ocean Coupling DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Large-Eddy Simulations of Tropical Convective Systems, the Boundary Layer, and Upper Ocean Coupling Eric D. Skyllingstad

More information

The Climatology of Clouds using surface observations. S.G. Warren and C.J. Hahn Encyclopedia of Atmospheric Sciences.

The Climatology of Clouds using surface observations. S.G. Warren and C.J. Hahn Encyclopedia of Atmospheric Sciences. The Climatology of Clouds using surface observations S.G. Warren and C.J. Hahn Encyclopedia of Atmospheric Sciences Gill-Ran Jeong Cloud Climatology The time-averaged geographical distribution of cloud

More information

Clouds, Haze, and Climate Change

Clouds, Haze, and Climate Change Clouds, Haze, and Climate Change Jim Coakley College of Oceanic and Atmospheric Sciences Earth s Energy Budget and Global Temperature Incident Sunlight 340 Wm -2 Reflected Sunlight 100 Wm -2 Emitted Terrestrial

More information

VAMOS Ocean-Cloud-Atmosphere-Land Study (VOCALS) Implementation Plan. Draft: January 13, Prepared by the VOCALS Scientific Working Group

VAMOS Ocean-Cloud-Atmosphere-Land Study (VOCALS) Implementation Plan. Draft: January 13, Prepared by the VOCALS Scientific Working Group VAMOS Ocean-Cloud-Atmosphere-Land Study (VOCALS) Implementation Plan Draft: January 13, 2005 Prepared by the VOCALS Scientific Working Group 1 1. Introduction and brief summary of science plan The VAMOS

More information

Part 2 Aircraft-based Observations

Part 2 Aircraft-based Observations Part 2 Aircraft-based Observations NSF C-130 CIRPAS Twin Otter FAAM BAe146 UK NEC Dornier 2028 Measuring microphysical, chemical and optical properties of aerosols aboard the NCAR/NSF C-130 during

More information

History of Earth Radiation Budget Measurements With results from a recent assessment

History of Earth Radiation Budget Measurements With results from a recent assessment History of Earth Radiation Budget Measurements With results from a recent assessment Ehrhard Raschke and Stefan Kinne Institute of Meteorology, University Hamburg MPI Meteorology, Hamburg, Germany Centenary

More information

The VAMOS Ocean-Cloud-Atmosphere-Land Study Regional Experiment (VOCALS-REx): goals, platforms, and field operations

The VAMOS Ocean-Cloud-Atmosphere-Land Study Regional Experiment (VOCALS-REx): goals, platforms, and field operations doi:10.5194/acp-11-627-2011 Author(s) 2011. CC Attribution 3.0 License. Atmospheric Chemistry and Physics The VAMOS Ocean-Cloud-Atmosphere-Land Study Regional Experiment (VOCALS-REx): goals, platforms,

More information

Southeast Pacific stratocumulus clouds, precipitation and boundary layer structure sampled along 20 S during VOCALS-REx

Southeast Pacific stratocumulus clouds, precipitation and boundary layer structure sampled along 20 S during VOCALS-REx Manuscript prepared for Atmos. Chem. Phys. with version 3. of the L A TEX class copernicus.cls. Date: 1 October 21 Southeast Pacific stratocumulus clouds, precipitation and boundary layer structure sampled

More information

Using volcanic eruptions to unlock the secrets of aerosol-cloud interactions. Jim Haywood

Using volcanic eruptions to unlock the secrets of aerosol-cloud interactions. Jim Haywood Using volcanic eruptions to unlock the secrets of aerosol-cloud interactions Jim Haywood Malavelle, F., et al., Strong constraints on aerosol-cloud interactions from volcanic eruptions, Nature, June 22

More information

Relevant timescales: convective events diurnal intraseasonal. 3 ocean-atmosphere communication methods: freshwater flux flux momentum flux

Relevant timescales: convective events diurnal intraseasonal. 3 ocean-atmosphere communication methods: freshwater flux flux momentum flux Radar Perspective on Air-Sea Interactions during DYNAMO Elizabeth Thompson; July 23 2013 Update Steve Rutledge, Brenda Dolan, Jim Moum, Aurelie Moulin, Chris Fairall, Bob Rilling, Mike Dixon, Scott Ellis,

More information

Observations of stratocumulus clouds and their effect on the eastern Pacific surface

Observations of stratocumulus clouds and their effect on the eastern Pacific surface 1 2 Observations of stratocumulus clouds and their effect on the eastern Pacific surface heat budget along 2 S 3 4 5 6 7 8 9 Simon P. de Szoeke Sandra Yuter David Mechem Chris W. Fairall Casey Burleyson

More information

Extratropical and Polar Cloud Systems

Extratropical and Polar Cloud Systems Extratropical and Polar Cloud Systems Gunilla Svensson Department of Meteorology & Bolin Centre for Climate Research George Tselioudis Extratropical and Polar Cloud Systems Lecture 1 Extratropical cyclones

More information

Southeast Pacific Stratocumulus Clouds, Precipitation and Boundary Layer Structure Sampled Along 20 S During VOCALS-REx

Southeast Pacific Stratocumulus Clouds, Precipitation and Boundary Layer Structure Sampled Along 20 S During VOCALS-REx Manuscript prepared for Atmos. Chem. Phys. Discuss. with version 2.0 of the LATEX class copernicus discussions.cls. Date: 11 June 2010 Southeast Pacific Stratocumulus Clouds, Precipitation and Boundary

More information

Robert Houze University of Washington (with contributions from B. Smull)

Robert Houze University of Washington (with contributions from B. Smull) Robert Houze University of Washington (with contributions from B. Smull) Winter MONEX Summer MONEX Presented at: International Conference on MONEX and its Legacy, 3-7 Feb 2005, New Delhi Johnson & Houze

More information

Downscaling Global Warming with a Regional Ocean- Atmosphere Model over the Tropical Atlantic

Downscaling Global Warming with a Regional Ocean- Atmosphere Model over the Tropical Atlantic Downscaling Global Warming with a Regional Ocean- Atmosphere Model over the Tropical Atlantic Role of equatorial ocean dynamics: equatorial upwelling and ocean mesoscale variability Hyodae Seo and Shang-Ping

More information

Aiguo Dai * and Kevin E. Trenberth National Center for Atmospheric Research (NCAR) $, Boulder, CO. Abstract

Aiguo Dai * and Kevin E. Trenberth National Center for Atmospheric Research (NCAR) $, Boulder, CO. Abstract 9.2 AMS 14 th Symposium on Global Change and Climate Variations, 9-13 Feb. 2003, Long Beach, CA. Diurnal Variations in the Community Climate System Model Aiguo Dai * and Kevin E. Trenberth National Center

More information

Climate Feedbacks from ERBE Data

Climate Feedbacks from ERBE Data Climate Feedbacks from ERBE Data Why Is Lindzen and Choi (2009) Criticized? Zhiyu Wang Department of Atmospheric Sciences University of Utah March 9, 2010 / Earth Climate System Outline 1 Introduction

More information

S. de Szoeke (NOAA), M. Kohler (ECMWF), T. Toniazzo (U. Reading, UK), and many others

S. de Szoeke (NOAA), M. Kohler (ECMWF), T. Toniazzo (U. Reading, UK), and many others R. Wood (U. Wash., Rex-PI), C. R. Mechoso (UCLA, Chair), C. Bretherton (U. Wash.), R. Weller (WHOI), C. Fairall (NOAA), H. Coe (Manchester U., UK), F. Straneo (WHOI), C. Grados (IMARPE, Peru), R. Garreaud

More information

Observational and Numerical Studies of the Boundary Layer, Cloud, and Aerosol Variability in the Southeast Pacific Coastal Marine Stratocumulus

Observational and Numerical Studies of the Boundary Layer, Cloud, and Aerosol Variability in the Southeast Pacific Coastal Marine Stratocumulus University of Miami Scholarly Repository Open Access Dissertations Electronic Theses and Dissertations 2012-05-01 Observational and Numerical Studies of the Boundary Layer, Cloud, and Aerosol Variability

More information

Upper-Ocean Processes under the Stratus Cloud Deck in the Southeast Pacific Ocean

Upper-Ocean Processes under the Stratus Cloud Deck in the Southeast Pacific Ocean JANUARY 2010 Z H E N G E T A L. 103 Upper-Ocean Processes under the Stratus Cloud Deck in the Southeast Pacific Ocean YANGXING ZHENG,* TOSHIAKI SHINODA, 1 GEORGE N. KILADIS,* JIALIN LIN, # E. JOSEPH METZGER,

More information

Large-Eddy Simulations of Tropical Convective Systems, the Boundary Layer, and Upper Ocean Coupling

Large-Eddy Simulations of Tropical Convective Systems, the Boundary Layer, and Upper Ocean Coupling DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Large-Eddy Simulations of Tropical Convective Systems, the Boundary Layer, and Upper Ocean Coupling Eric D. Skyllingstad

More information

A perturbed physics ensemble climate modeling. requirements of energy and water cycle. Yong Hu and Bruce Wielicki

A perturbed physics ensemble climate modeling. requirements of energy and water cycle. Yong Hu and Bruce Wielicki A perturbed physics ensemble climate modeling study for defining satellite measurement requirements of energy and water cycle Yong Hu and Bruce Wielicki Motivation 1. Uncertainty of climate sensitivity

More information

Lecture 8: Climate Modeling

Lecture 8: Climate Modeling Lecture 8: Climate Modeling How to Build a Climate Model The climate is governed by many complex physical, chemical, and biological processes and their interactions. Building a climate model needs to consider

More information

Lecture 14. Marine and cloud-topped boundary layers Marine Boundary Layers (Garratt 6.3) Marine boundary layers typically differ from BLs over land

Lecture 14. Marine and cloud-topped boundary layers Marine Boundary Layers (Garratt 6.3) Marine boundary layers typically differ from BLs over land Lecture 14. Marine and cloud-topped boundary layers Marine Boundary Layers (Garratt 6.3) Marine boundary layers typically differ from BLs over land surfaces in the following ways: (a) Near surface air

More information

Variability in Global Top-of-Atmosphere Shortwave Radiation Between 2000 And 2005

Variability in Global Top-of-Atmosphere Shortwave Radiation Between 2000 And 2005 Variability in Global Top-of-Atmosphere Shortwave Radiation Between 2000 And 2005 Norman G. Loeb NASA Langley Research Center Hampton, VA Collaborators: B.A. Wielicki, F.G. Rose, D.R. Doelling February

More information

Development of a High-Resolution Coupled Atmosphere-Ocean-Land General Circulation Model for Climate System Studies

Development of a High-Resolution Coupled Atmosphere-Ocean-Land General Circulation Model for Climate System Studies Chapter 1 Earth Science Development of a High-Resolution Coupled Atmosphere-Ocean-Land General Circulation Model for Climate System Studies Project Representative Tatsushi Tokioka Frontier Research Center

More information

GEWEX Cloud System Study (GCSS)

GEWEX Cloud System Study (GCSS) GEWEX Cloud System Study (GCSS) The goal of GCSS is to improve the parameterization of cloud systems in GCMs (global climate models) and NWP (numerical weather prediction) models through improved physical

More information

UC Irvine Faculty Publications

UC Irvine Faculty Publications UC Irvine Faculty Publications Title A linear relationship between ENSO intensity and tropical instability wave activity in the eastern Pacific Ocean Permalink https://escholarship.org/uc/item/5w9602dn

More information

Lecture 3. Background materials. Planetary radiative equilibrium TOA outgoing radiation = TOA incoming radiation Figure 3.1

Lecture 3. Background materials. Planetary radiative equilibrium TOA outgoing radiation = TOA incoming radiation Figure 3.1 Lecture 3. Changes in planetary albedo. Is there a clear signal caused by aerosols and clouds? Outline: 1. Background materials. 2. Papers for class discussion: Palle et al., Changes in Earth s reflectance

More information

Fast and Slow Response of Sea ice and the Southern Ocean to Ozone Depletion

Fast and Slow Response of Sea ice and the Southern Ocean to Ozone Depletion Fast and Slow Response of Sea ice and the Southern Ocean to Ozone Depletion Annual Minimum Sea ice extent 1979-2013 10 6 km 2 Arctic September Antarctic February Data from in passive microwave satellite

More information

Standalone simulations: CAM3, CAM4 and CAM5

Standalone simulations: CAM3, CAM4 and CAM5 Standalone simulations: CAM3, and CAM5 CAM5 Model Development Team Cécile Hannay, Rich Neale, Andrew Gettelman, Sungsu Park, Joe Tribbia, Peter Lauritzen, Andrew Conley, Hugh Morrison, Phil Rasch, Steve

More information

Can dust cause droughts?

Can dust cause droughts? Can dust cause droughts? Dust and sea surface temperature forcing of the 1930 s Dust bowl Cook et al., GRL 2008 Impact of desert dust radiative forcing on Sahel precipitation: Radiative Importance of dust

More information

Arctic climate projections and progress towards a new CCSM. Marika Holland NCAR

Arctic climate projections and progress towards a new CCSM. Marika Holland NCAR Arctic climate projections and progress towards a new CCSM Marika Holland NCAR The Arctic is changing! Loss of Sept Arctic Sea Ice 2002 Loss of about 8% per decade Or >20% since 1979 (Courtesy I. Rigor

More information

Sungsu Park, Chris Bretherton, and Phil Rasch

Sungsu Park, Chris Bretherton, and Phil Rasch Improvements in CAM5 : Moist Turbulence, Shallow Convection, and Cloud Macrophysics AMWG Meeting Feb. 10. 2010 Sungsu Park, Chris Bretherton, and Phil Rasch CGD.NCAR University of Washington, Seattle,

More information

P1.3 DIURNAL VARIABILITY OF THE CLOUD FIELD OVER THE VOCALS DOMAIN FROM GOES IMAGERY. CIMMS/University of Oklahoma, Norman, OK 73069

P1.3 DIURNAL VARIABILITY OF THE CLOUD FIELD OVER THE VOCALS DOMAIN FROM GOES IMAGERY. CIMMS/University of Oklahoma, Norman, OK 73069 P1.3 DIURNAL VARIABILITY OF THE CLOUD FIELD OVER THE VOCALS DOMAIN FROM GOES IMAGERY José M. Gálvez 1, Raquel K. Orozco 1, and Michael W. Douglas 2 1 CIMMS/University of Oklahoma, Norman, OK 73069 2 NSSL/NOAA,

More information

Interannual variability of top-ofatmosphere. CERES instruments

Interannual variability of top-ofatmosphere. CERES instruments Interannual variability of top-ofatmosphere albedo observed by CERES instruments Seiji Kato NASA Langley Research Center Hampton, VA SORCE Science team meeting, Sedona, Arizona, Sep. 13-16, 2011 TOA irradiance

More information

Climatology of stratocumulus cloud morphologies: microphysical properties and radiative effects

Climatology of stratocumulus cloud morphologies: microphysical properties and radiative effects Atmos. Chem. Phys., 1, 669 6716, 1 www.atmos-chem-phys.net/1/669/1/ doi:1.19/acp-1-669-1 Author(s) 1. CC Attribution 3. License. Climatology of stratocumulus cloud morphologies: microphysical properties

More information

Interannual Variations of Arctic Cloud Types:

Interannual Variations of Arctic Cloud Types: Interannual Variations of Arctic Cloud Types: Relationships with Sea Ice and Surface Temperature Ryan Eastman Stephen Warren University of Washington Department of Atmospheric Sciences Changes in Arctic

More information

Convection Trigger: A key to improving GCM MJO simulation? CRM Contribution to DYNAMO and AMIE

Convection Trigger: A key to improving GCM MJO simulation? CRM Contribution to DYNAMO and AMIE Convection Trigger: A key to improving GCM MJO simulation? CRM Contribution to DYNAMO and AMIE Xiaoqing Wu, Liping Deng and Sunwook Park Iowa State University 2009 DYNAMO Workshop Boulder, CO April 13-14,

More information

Interannual variability of the upper ocean in the southeast Pacific stratus cloud region

Interannual variability of the upper ocean in the southeast Pacific stratus cloud region Interannual variability of the upper ocean in the southeast Pacific stratus cloud region Toshiaki Shinoda 1 and Jialin Lin 2 1 Naval Research Laboratory, Stennis Space Center, Mississippi 2 Department

More information

An Interconnected Planet

An Interconnected Planet An Interconnected Planet How Clouds, Aerosols, and the Ocean Cause Distant Rainfall Anomalies Dargan M. W. Frierson University of Washington CESM Workshop, 6-15-15 New Connections Recent research has uncovered

More information

The Regional Arctic System Model (RASM) for Studying High Resolution Climate Changes in the Arctic

The Regional Arctic System Model (RASM) for Studying High Resolution Climate Changes in the Arctic The Regional Arctic System Model (RASM) for Studying High Resolution Climate Changes in the Arctic Mark W. Seefeldt, John J. Cassano, Alice K. Duvivier, and Mimi H. Hughes University of Colorado Boulder

More information

Cloud feedbacks on dynamics and SST in an equatorial mock-walker circulation

Cloud feedbacks on dynamics and SST in an equatorial mock-walker circulation Cloud feedbacks on dynamics and SST in an equatorial mock-walker circulation Equator (f=0) p W Pacific Warm SST x E Pacific Colder SST Ocean heat loss Very cold deep ocean Understand cloud feedbacks on:

More information

Climate Dynamics (PCC 587): Clouds and Feedbacks

Climate Dynamics (PCC 587): Clouds and Feedbacks Climate Dynamics (PCC 587): Clouds and Feedbacks D A R G A N M. W. F R I E R S O N U N I V E R S I T Y O F W A S H I N G T O N, D E P A R T M E N T O F A T M O S P H E R I C S C I E N C E S D A Y 7 : 1

More information

State of the Community Climate System Model

State of the Community Climate System Model State of the Community Climate System Model Peter Gent Chairman CCSM Scientific Steering Committee gent@ucar.edu Recent Science Highlights CCSM IJHPCA Special Issue Objectives Describe SE for climate models

More information

Observations of Stratocumulus Clouds and Their Effect on the Eastern Pacific Surface Heat Budget along 208S

Observations of Stratocumulus Clouds and Their Effect on the Eastern Pacific Surface Heat Budget along 208S 8542 J O U R N A L O F C L I M A T E VOLUME 25 Observations of Stratocumulus Clouds and Their Effect on the Eastern Pacific Surface Heat Budget along 208S SIMON P. DE SZOEKE,* SANDRA YUTER, 1 DAVID MECHEM,

More information

Comparison of MODIS cloud microphysical properties with in-situ measurements over the Southeast Pacific

Comparison of MODIS cloud microphysical properties with in-situ measurements over the Southeast Pacific Atmos. Chem. Phys., 12, 11261 11273, 2012 doi:10.5194/acp-12-11261-2012 Author(s) 2012. CC Attribution 3.0 License. Atmospheric Chemistry and Physics Comparison of MODIS cloud microphysical properties

More information

Air-Sea Coupling in an Eastern Boundary Current Region

Air-Sea Coupling in an Eastern Boundary Current Region Air-Sea Coupling in an Eastern Boundary Current Region Eric D. Skyllingstad CEOAS, Oregon State University Roger M. Samelson D. B. Chelton, A. Kurapov CEOAS, Oregon State University N. Perlin RSMAS, University

More information

NOAA Climate Program and CPPA Overview (Climate Prediction Program for the Americas)

NOAA Climate Program and CPPA Overview (Climate Prediction Program for the Americas) NOAA Climate Program and CPPA Overview (Climate Prediction Program for the Americas) Jin Huang NOAA Climate Program Office June 3, 2009 NOAA Climate Goal Understand Climate Variability and Change to Enhance

More information

Parameterizing large-scale circulations based on the weak temperature gradient approximation

Parameterizing large-scale circulations based on the weak temperature gradient approximation Parameterizing large-scale circulations based on the weak temperature gradient approximation Bob Plant, Chimene Daleu, Steve Woolnough and thanks to GASS WTG project participants Department of Meteorology,

More information

Aerosol-Cloud-Climate Interaction: A Case Study from the Indian Ocean. Sagnik Dey

Aerosol-Cloud-Climate Interaction: A Case Study from the Indian Ocean. Sagnik Dey Aerosol-Cloud-Climate Interaction: A Case Study from the Indian Ocean Sagnik Dey Centre for Atmospheric Sciences Indian Institute of Technology Delhi sagnik@cas.iitd.ac.in Content Background and Motivation

More information

Polar regions Temperate Regions Tropics High ( cirro ) 3-8 km 5-13 km 6-18 km Middle ( alto ) 2-4 km 2-7 km 2-8 km Low ( strato ) 0-2 km 0-2 km 0-2 km

Polar regions Temperate Regions Tropics High ( cirro ) 3-8 km 5-13 km 6-18 km Middle ( alto ) 2-4 km 2-7 km 2-8 km Low ( strato ) 0-2 km 0-2 km 0-2 km Clouds and Climate Clouds (along with rain, snow, fog, haze, etc.) are wet atmospheric aerosols. They are made up of tiny spheres of water from 2-100 m which fall with terminal velocities of a few cm/sec.

More information

Today s Lecture: Land, biosphere, cryosphere (All that stuff we don t have equations for... )

Today s Lecture: Land, biosphere, cryosphere (All that stuff we don t have equations for... ) Today s Lecture: Land, biosphere, cryosphere (All that stuff we don t have equations for... ) 4 Land, biosphere, cryosphere 1. Introduction 2. Atmosphere 3. Ocean 4. Land, biosphere, cryosphere 4.1 Land

More information

Satellite-based estimate of global aerosol-cloud radiative forcing by marine warm clouds

Satellite-based estimate of global aerosol-cloud radiative forcing by marine warm clouds SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO2214 Satellite-based estimate of global aerosol-cloud radiative forcing by marine warm clouds Y.-C. Chen, M. W. Christensen, G. L. Stephens, and J. H. Seinfeld

More information

Satellite and diagnostic model estimates of precipitation susceptibility in low-level, marine stratocumulus

Satellite and diagnostic model estimates of precipitation susceptibility in low-level, marine stratocumulus JOURNAL OF GEOPHYSICAL RESEARCH, VOL.???, XXXX, DOI:.9/, 3 Satellite and diagnostic model estimates of precipitation susceptibility in low-level, marine stratocumulus Christopher. R. Terai, Robert Wood,

More information

An Overview of NRCM Research and Lessons Learned

An Overview of NRCM Research and Lessons Learned An Overview of NRCM Research and Lessons Learned L. Ruby Leung Pacific Northwest National Laboratory With NCAR MMM/CGD scientists, students (U. Miami, Georgia Tech), and visitors (CMA and Taiwan) The NRCM

More information

Evaluation of Forecasted Southeast Pacific Stratocumulus in the NCAR, GFDL, and ECMWF Models

Evaluation of Forecasted Southeast Pacific Stratocumulus in the NCAR, GFDL, and ECMWF Models 1JUNE 2009 H A N N A Y E T A L. 2871 Evaluation of Forecasted Southeast Pacific Stratocumulus in the NCAR, GFDL, and ECMWF Models CÉCILE HANNAY, DAVID L. WILLIAMSON, JAMES J. HACK, JEFFREY T. KIEHL, AND

More information

ATOC 5051 INTRODUCTION TO PHYSICAL OCEANOGRAPHY. Lecture 19. Learning objectives: develop a physical understanding of ocean thermodynamic processes

ATOC 5051 INTRODUCTION TO PHYSICAL OCEANOGRAPHY. Lecture 19. Learning objectives: develop a physical understanding of ocean thermodynamic processes ATOC 5051 INTRODUCTION TO PHYSICAL OCEANOGRAPHY Lecture 19 Learning objectives: develop a physical understanding of ocean thermodynamic processes 1. Ocean surface heat fluxes; 2. Mixed layer temperature

More information

Development of a Coupled Atmosphere-Ocean-Land General Circulation Model (GCM) at the Frontier Research Center for Global Change

Development of a Coupled Atmosphere-Ocean-Land General Circulation Model (GCM) at the Frontier Research Center for Global Change Chapter 1 Atmospheric and Oceanic Simulation Development of a Coupled Atmosphere-Ocean-Land General Circulation Model (GCM) at the Frontier Research Center for Global Change Project Representative Tatsushi

More information

Susan Bates Ocean Model Working Group Science Liaison

Susan Bates Ocean Model Working Group Science Liaison Susan Bates Ocean Model Working Group Science Liaison Climate Simulation Laboratory (CSL) Accelerated Scientific Discovery (ASD) NCAR Strategic Capability (NSC) Climate Process Teams (CPTs) NSF Earth System

More information

Diagnosing Southeast Tropical Atlantic SST and Ocean. Circulation Biases in the CMIP5 Ensemble

Diagnosing Southeast Tropical Atlantic SST and Ocean. Circulation Biases in the CMIP5 Ensemble 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 Diagnosing Southeast Tropical Atlantic SST and Ocean Circulation Biases in the CMIP5 Ensemble Zhao Xu Physical Oceanography Laboratory, Ocean University of China Department

More information

Ship-based measurements of cloud microphysics and PBL properties in precipitating trade cumulus clouds during RICO

Ship-based measurements of cloud microphysics and PBL properties in precipitating trade cumulus clouds during RICO Ship-based measurements of cloud microphysics and PBL properties in precipitating trade cumulus clouds during RICO Allen White and Jeff Hare, University of Colorado/CIRES Bruce Albrecht and Pavlos Kolias,

More information

Comparisons of satellites liquid water estimates to ECMWF and GMAO analyses, 20th century IPCC AR4 climate simulations, and GCM simulations

Comparisons of satellites liquid water estimates to ECMWF and GMAO analyses, 20th century IPCC AR4 climate simulations, and GCM simulations GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L19710, doi:10.1029/2008gl035427, 2008 Comparisons of satellites liquid water estimates to ECMWF and GMAO analyses, 20th century IPCC AR4 climate simulations, and

More information

Moist static energy budget diagnostics for. monsoon research. H. Annamalai

Moist static energy budget diagnostics for. monsoon research. H. Annamalai Moist static energy budget diagnostics for monsoon research H. Annamalai JJAS Precipitation and SST Climatology I III II Multiple regional heat sources - EIO and SPCZ still experience high precipitation

More information

The TRMM Precipitation Radar s View of Shallow, Isolated Rain

The TRMM Precipitation Radar s View of Shallow, Isolated Rain OCTOBER 2003 NOTES AND CORRESPONDENCE 1519 The TRMM Precipitation Radar s View of Shallow, Isolated Rain COURTNEY SCHUMACHER AND ROBERT A. HOUZE JR. Department of Atmospheric Sciences, University of Washington,

More information

Intermittency in precipitation: duration, frequency, intensity and amounts using hourly data

Intermittency in precipitation: duration, frequency, intensity and amounts using hourly data Intermittency in precipitation: duration, frequency, intensity and amounts using hourly data Kevin E Trenberth with Yongxin Zhang and Maria Gehne NCAR How should rainfall change as climate changes? Usually

More information