Does anyone believe that this feedback loop works as advertised?

Slides:



Advertisements
Similar presentations
Overview: C. Roberto Mechoso Clouds and Aerosol: Chris Bretherton OceanFluxes: Bob Weller Aerosol and Biology: Barry Huebert Discussions on Program Requirements.
Advertisements

Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Section highlights Organic Aerosol and Field Studies.
Clouds and Climate: Forced Changes to Clouds SOEE3410 Ken Carslaw Lecture 4 of a series of 5 on clouds and climate Properties and distribution of clouds.
Anthropogenic Aerosol – A Cause Of The Weekend Effect? A significant weekly cycle has been found in diurnal temperature range (DTR). A candidate for causing.
Mean annual temperature (°F) Mean annual precipitation (inches)
SULFATE & THE CLAW HYPOTHESIS. TOPICS FOR TODAY 1.The Sulfur Cycle & Sources of Sulfate 2.The CLAW hypothesis 3.How might sulfate concentrations be affected.
Ultrafine Particles and Climate Change Peter J. Adams HDGC Seminar November 5, 2003.
Implementation of Sulfate and Sea-Salt Aerosol Microphysics in GEOS-Chem Hi everyone. My name is Win Trivitayanurak… I’m a PhD student working with Peter.
PMEL Atmospheric Chemistry Climate Air Quality 1.The Scientists 2.History 3.Highlights of results 4.Near future plans.
© Crown copyright Met Office Met Office VOCALS activities and interests Phil Brown, Steve Abel and others 29 th July 2008 VOCALS-UK Planning Meeting.
SETTING THE STAGE FOR: BIOSPHERE, CHEMISTRY, CLIMATE INTERACTIONS.
Aerosols and climate Rob Wood, Atmospheric Sciences.
Clouds and Climate: Forced Changes to Clouds SOEE3410 Ken Carslaw Lecture 4 of a series of 5 on clouds and climate Properties and distribution of clouds.
Robert Wood, University of Washington many contributors VOCALS Regional Experiment (REx) Goals and Hypotheses.
Revisit science priorities for CalWater 2015 – ACAPEX L.R. Leung, PNNL.
-integral to VOCALS objectives -we want to do the best we can: * marine stratus over ocean is the idealization many retrievals of warm cloud properties.
Aerosol Microphysics: Plans for GEOS-CHEM
The Provenance of Sulfur that Becomes Non-Seasalt Sulfate (NSS) Barry J Huebert, Rebecca M Simpson, Steven G Howell, and Byron W Blomquist
Proposal for a Research Infrastructure for Advanced Aerosol Observations and Capacity Building in China Alfred WIEDENSOHLER Leibniz Institute for Tropospheric.
Improving Black Carbon (BC) Aging in GEOS-Chem Based on Aerosol Microphysics: Constraints from HIPPO Observations Cenlin He Advisers: Qinbin Li, Kuo-Nan.
Surface and Boundary-Layer Fluxes during the DYNAMO Field Program C. Fairall, S. DeSzoeke, J. Edson, + Surface cloud radiative forcing (CF) Diurnal cycles.
Equatorial Pacific primary productivity: Spatial and temporal variability and links to carbon cycling Pete Strutton College of Oceanic and Atmospheric.
Biosphere/Atmosphere Interactions in the Tropics.
Fluxes of bio-available iron to the ocean ○ Akinori Ito Research Institute for Global Change, JAMSTEC Yan Feng Scripps Institution of Oceanography, University.
Aerosol-Cloud Interactions and Radiative Forcing: Modeling and Observations Graham Feingold 1, K. S. Schmidt 2, H. Jiang 3, P. Zuidema 4, H. Xue 5, P.
Department of Environmental Earth System Science Stanford University
Group proposal Aerosol, Cloud, and Climate ( EAS 8802) April 24 th, 2006 Does Asian dust play a role as CCN? Gill-Ran Jeong, Lance Giles, Matthew Widlansky.
Boundary Layer Clouds.
Robert Wood, Atmospheric Sciences, University of Washington The importance of precipitation in marine boundary layer cloud.
VOCALS Status Report Robert Wood, University of Washington on behalf of the VOCALS Scientific Working Group.
Free troposphere as a major source of CCN for the equatorial pacific boundary layer: long-range transport and teleconnections Presented by: Stephen Noble.
A Seven-Cruise Sample of Clouds, Radiation, and Surface Forcing in the Equatorial Eastern Pacific J. E. Hare, C. W. Fairall, T. Uttal, D. Hazen NOAA Environmental.
An Interactive Aerosol-Climate Model based on CAM/CCSM: Progress and challenging issues Chien Wang and Dongchul Kim (MIT) Annica Ekman (U. Stockholm) Mary.
Multidisciplinary drifting Observatory for the Study of Arctic Climate
Using WRF-Chem to understand interactions between synoptic and microphysical variability during VOCALS Rhea George, Robert Wood University of Washington.
PAPERSPECIFICS OF STUDYFINDINGS Kohler, 1936 (“The nucleus in and the growth of hygroscopic droplets”) Evaporate 2kg of hoar-frost and determined Cl content;
FIVE CHALLENGES IN ATMOSPHERIC COMPOSITION RESEARCH 1.Exploit satellite and other “top-down” atmospheric composition data to quantify emissions and export.
Charlson et al.,Nature, 326, , CLAW Hypothesis DMS as an Integrator of Dynamic, Chemical, and Biological Processes during VOCALS Barry Huebert.
Aerosol 1 st indirect forcing in the coupled CAM-IMPACT model: effects from primary-emitted particulate sulfate and boundary layer nucleation Minghuai.
VOCALS-REx Flight Planning. VOCALS Regional Experiment (REx) VOCALS-Rex will collect datasets required to address a set of issues that are organized into.
ATS 621 Fall 2012 Lecture 5. Back to the Box Model…. Example: strat-trop exchange.
Science Working Group: C. R. Mechoso (Chair) Atmosphere: C. Bretherton, R. Garreaud Ocean: B. Weller, J. McWilliams Field Experiment (US): C. Fairall,
Chemistry-climate interactions in CCSM
Marine stratocumulus clouds
Future CO2 Forcing Climate Sensitivity – Feedbacks
Stratocumulus cloud thickening beneath layers of absorbing smoke aerosol – Wilcox, 2010 The semi-direct aerosol effect: Impact of absorbing aerosols.
Condensation in the Atmosphere
H. Morrison, A. Gettelman (NCAR) , S. Ghan (PNL)
Aerosol Physics & Climate
What are the causes of GCM biases in cloud, aerosol, and radiative properties over the Southern Ocean? How can the representation of different processes.
Natural Causes of Climate Change
Robert Wood, University of Washington
TOWARDS AN AEROSOL CLIMATOLOGY
Upper Troposphere and Lower Stratosphere Break out
Boundary layer depth, entrainment, decoupling, and clouds over the eastern Pacific Ocean Robert Wood, Atmospheric Sciences, University of Washington.
Coastal CO2 fluxes from satellite ocean color, SST and winds
Roberto Mechoso and I. Richter
The Southeast Pacific Climate
AEROSOLS REDUCE ATMOSPHERIC OXIDATION
+ = Climate Responses to Biomass Burning Aerosols over South Africa
Simple CCN budget in the MBL
FOUR MAJOR RESEARCH CHALLENGES FOR THE SECOND DECADE OF THE USGCRP
NSF C-130 Platform Report MISSIONS INSTRUMENTS Robert Wood
Control of Cloud Droplet Concentration in Marine Stratocumulus Clouds
Aerosol Optical Thickness
The importance of precipitation in marine boundary layer cloud
VOCALS Open Ocean: Science and Logistics
Breakout Group B: summary Aerosol-Cloud-Precipitation Science Objectives Chemistry/aerosol distinct differences in key terms in aerosol budgets in different.
The Southeast Pacific Climate
Presentation transcript:

Does anyone believe that this feedback loop works as advertised? 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, Lovelock, Andreae, and Warren, Oceanic phytoplankton, atmospheric sulfur, cloud albedo and climate, Nature, 326, 655-661, 1987.

Neither can be understood in isolation from the other. The CLAW Hypothesis DMS fluxes probably control the growth of aerosols into the CCN size range. These CCN help control the radiative properties of stratocumulus clouds. Although CLAW has not been rigorously proven, it is extremely likely that biological processes are linked to cloud properties via sulfur-containing aerosols. Neither can be understood in isolation from the other. CLAW Hypothesis

What role do aerosols play in creating these pockets of open cells, POCs? To improve models of this region, we need to quantify the factors controlling clouds and radiation. 2-300 Wm-2 Difference!

Drizzle Removal > Nucleation > DMS-Controlled Growth This aerosol data from an EPIC cruise shows the loss of aerosols when a POC passes overhead. Tony Clarke observed this re-growth from freshly-nucleated particles in the Eastern Pacific MBL during PEM-Tropics. Drizzle Removal > Nucleation > DMS-Controlled Growth is one plausible explanation for several-day POC lifetimes. How much of the recovery is from entrainment vs growth? POC Data courtesy Fairall & Collins

The upwelling of cold, nutrient rich deep water creates gradients in biological productivity that should translate into gradients of DMS emissions and other . We can exploit these gradients to study the factors controlling fluxes, aerosol chemistry, and cloud properties.

We propose to study this chemistry from both ships and aircraft. In the remote marine atmosphere the supply of DMS and its oxidation mechanisms limit the rates of new particle nucleation and growth. These processes probably control the re-filling of POCs with clouds. Iodine, ammonia, and organics may also play a role. We propose to study this chemistry from both ships and aircraft.

Our new ability to directly measure both DMS and SO2 fluxes (and entrainment rates!) by eddy covariance‡ enables us to constrain the sulfur budget as never before. By quantifying the fluxes and oxidation rates, we can put reasonable bounds on aerosol growth rates. ‡We are proposing to measure fluxes both from the Ron Brown (time series) and from the C-130 (vertical profiles, across the inversion, and in and out of POCs). Huebert et al., GRL, doi: 10.1029/2004GL021567, 2004

For the CLIVAR/VOCALS Aerosol/Cloud Objectives, what measurements are needed? Aerosol temporal and spatial variation scales Fast measurements to very small sizes, with composition, Lidar Aerosol Nucleation Ultrafine CN, SMPS, precursor gases (DMS, SO2, I?) Indirect effect sensitivity Mass and composition vs size (incl. sulfate and organic carbon), CCN Aerosol vs cloud fraction Fast number vs size, composition, CVI, CCN Particle sources and sinks Precursor gases, sulfate, OC, EC, CW composition

Testing the DMSgas to CCN parts would require Lagrangian observations. SOLAS: This is an excellent natural laboratory to test the CLAW Hypothesis Possible SOLAS experiments include examining the impact of POC-driven irradiance changes on SST, productivity, and DMS fluxes, all the unshaded parts of this diagram. Testing the DMSgas to CCN parts would require Lagrangian observations. CLAW Hypothesis Nature, 326, 655-661, 1987.

POCs should change irradiance (and thus SST) enough to allow a test of the light/temp>biology>DMS emissions parts of the CLAW Hypothesis. (A SOLAS experiment along these lines might be proposed for 2008 or 2009.)

IGBP’s Surface Ocean Lower Atmosphere Study (SOLAS) has formally agreed to collaborate with CLIVAR on VOCALS. http://www.uea.ac.uk/env/solas/ The SEP cloud/radiation system is clearly coupled to the marine biological system via sulfur emissions and aerosol microphysics. We have an opportunity to study them in concert, leveraging the contributions of other programs to make this affordable to the sponsoring agencies.