Institute for Climate and Atmospheric Science (ICAS)

Slides:



Advertisements
Similar presentations
Modelling Capabilities for Aerosols and Climate at CCCma Knut von Salzen Canadian Centre for Climate Modelling and Analysis (CCCma)‏ Environment Canada,
Advertisements

Cirrus cloud evolution and radiative characteristics By Sardar AL-Jumur Supervisor Steven Dobbie.
2. Formation of Cloud droplets
Simulation of Cloud Droplets in Parameterized Shallow Cumulus During RICO and ICARTT Knut von Salzen 1, Richard Leaitch 2, Nicole Shantz 3, Jonathan Abbatt.
What are aerosols ? Aerosol is a collection of particles suspended in the air, they range in size from 0.01 microns to several tens of microns.
The Scientific Method: Real examples Monika V Sikand Ph.d Student Stevens Institute of Technology Department of Physics Light and Life Laboratory Hoboken.
Impacts of Climate Change on Physical Systems PPT
One Hundred Years of Arctic Surface Temperature Variation Fyfe 1, von Salzen 1, Gillett 1, Arora 1, Flato 1 & McConnell 2 1 Canadian Centre for Climate.
5. Formation and Growth of Ice Crystals
Modeling BC Sources and Sinks - research plan Charles Q. Jia and Sunling Gong University of Toronto and Environment 1 st annual NETCARE workshop.
Different heterogeneous routes of the formation of atmospheric ice Anatoli Bogdan Institute of Physical Chemistry, University of Innsbruck Austria and.
Black Carbon in Snow: Treatment and Results Mark Flanner 1 Charlie Zender 2 Jim Randerson 2 Phil Rasch 1 1 NCAR 2 University of California at Irvine.
Aerosol Microphysics: Plans for GEOS-CHEM
(Impacts are Felt on Scales from Local to Global) Aerosols Link Climate, Air Quality, and Health: Dirtier Air and a Dimmer Sun Emissions Impacts == 
Clouds, Aerosols and Precipitation GRP Meeting August 2011 Susan C van den Heever Department of Atmospheric Science Colorado State University Fort Collins,
11 The potential impact of mineral dust on cirrus (and other) cloud formation: a trajectory modeling perspective Aldona Wiącek * and Thomas Peter ETH,
CLIMATE CHANGES KAMIL JAGIEŁŁO. CLIMATE CHANGES Climate change result’s from factors such as the amount of incoming solar radiation or internal factors.
The effects of wind-shear on cirrus: a large eddy model (LEM) and radar case study Gourihar Kulkarni* and Steven Dobbie Institute for Climate and Atmospheric.
Fanglin Yang Work Done at Climate Research Group
Carbonaceous aerosols – a global modeling view Betty Croft and Ulrike Lohmann * Department of Physics and Atmospheric Science Dalhousie University, Halifax,
Ice in the Atmosphere W+H 6.5; S+P Ch. 17 Start with some terminology –Warm clouds = T > 0 ºC (= K) –Cold clouds = T < 0 ºC Cold clouds may or may.
Individual-particle studies of cloud droplet residues and ambient aerosols in RICO: the effect of particle size, composition, surface properties, and mixing.
Cloud Microphysics Liz Page NWS/COMET Hydromet February 2000.
Black Carbon Ageing in the CCCma GCM Betty Croft and Ulrike Lohmann Department of Physics and Atmospheric Science Dalhousie University, Halifax, N.S. Canada.
Guy Cascella, in association with MPO531, presents: Featuring: African dust aerosols as atmospheric nuclei, DeMott et al, 2003 Chemical characteristics.
Particle Size, Water Path, and Photon Tunneling in Water and Ice Clouds ARM STM Albuquerque Mar Sensitivity of the CAM to Small Ice Crystals.
Jeng K. Rongchai FETE Conference 21 July 2011.
WGNE Systematic Errors Workshop: Grand and Other Challenges Christian Jakob, ARC Centre of Excellence for Climate System Science, Monash University, Melbourne,
MIT Microstructural Evolution in Materials 12: Nucleation
Environmental Physics Laboratory, Institute of Physics Belgrade
The CLOUD experiment Cosmics Leaving Outdoor Droplets
Formation of cirrus cloud by glassy aerosols
Process work on the coupling of
Characterizing multispectral vertical profiles of aerosol extinction with surface-based measurements This presentation links surface-based particle counts,
Clouds and Large Model Grid Boxes
AM and ChemClim WG - February, 2008
Simulation of the Arctic Mixed-Phase Clouds
SFB 641 The SFB Laboratory contributes 2 different techniques for the measurements of ice nuclei to VI Aerosol-Cloud Interaction: 1. in situ-measurements.
Effects of 3D radiation on cloud evolution
The representation of ice hydrometeors in ECHAM-HAM
Remote Sensing of Aerosols
By Gourihar Kulkarni Steven Dobbie Mike Smith Jim McQuaid
Remote Sensing of Aerosols
ATOC 4720 class19 Thunderstorms 1. Growth of clouds droplets in
Alberto Sánchez-Marroquín, S. T. Parker, J. Trembath, I. Burke, J. B
Freezing Pathways Homogenous  Deposition  Contact  Condensation 
Cloud Dynamics and Microphysics Group
Research Scientist, Colorado State University
AEROSOLS REDUCE ATMOSPHERIC OXIDATION
Influences of Wet Scavenging on Aerosol Concentrations and Deposition in the ECHAM5-HAM Global Climate Model Betty Croft1 Ulrike.
Tore Furevik Geophysical Institute, University of Bergen
大气圈地球化学及其环境效益.
Ice nucleation experimental and modelling research (Murray and Dobbie)
Oxygen isotope tracers of atmospheric sulfur/oxidant chemistry
GCM activities in Ulrike Lohmann’s group
Evolution of tropical cirrus clouds.
John Marsham and Steven Dobbie
A. Gettelman, X. Liu, H. Morrison, S. Ghan
Turbulence-induced broadening of cloud-droplet size distributions: Implications for aerosol effects on climate Tuesday, April 25, :00-12:00 Noon.
The radiative properties of inhomogeneous cirrus clouds
Development of Ice Nucleation Chamber
Effects of 3D radiation on cloud evolution
PHY Lecture 16 Lidar remote sensing.
Cirrus microphysical and radiative properties
Breakout Group B: summary Aerosol-Cloud-Precipitation Science Objectives Chemistry/aerosol distinct differences in key terms in aerosol budgets in different.
 Return to #1 or proceed forward
Fig. 8. Mean annual cycle of the difference in mean SAT north of 60°N between the 5 simulations with 500 ppm pCO2 and αmin = 0.5, and the 5 with 400 ppm.
Fig. 2 Reconstructed global mean temperatures.
Cloud Formation.
Presentation transcript:

Institute for Climate and Atmospheric Science (ICAS) Mineral Dust Ice Nucleation Experiments Steven Dobbie, Jim McQuaid Gourihar Kulkarni (PhD 2007), Figure 1. The TGDC is housed in the Environmental Cold room at ICAS Aerosol Facility, ICAS Key points of new chamber design: Static diffusion chamber Observation of nucleation events of individual particles Flexibility to expose individual particles to a range of supersaturations. Stable temperature control Designed for process studies

Mineral Dust Ice Nucleation Experiments Institute for Climate and Atmospheric Science (ICAS) Mineral Dust Ice Nucleation Experiments Figure 2. SEM of Saharan mineral dust Gourihar Kulkarni (PhD, 2007) studied the onset nucleation super-saturation of Saharan mineral dust with temperature (Kulkarni et al., Submitted to AMT, 2008)

Current & Future Nucleation Experiments Institute for Climate and Atmospheric Science (ICAS) Current & Future Nucleation Experiments - Homogeneous nucleation of glassy particles. Theo Wilson, Chem PhD student with Ben Murray (Chem) and Steven Dobbie (ICAS). Memory effect of IN particles. NERC grant application (Dec 1, 2008), collaboration of Ben Murray (Chem) and Steven Dobbie (ICAS). Gas inlet Sub-sat stage Water vapour bath Ice nucleation chamber

Institute for Climate and Atmospheric Science (ICAS) Aerosol Modelling (Dobbie): Collaborative link with Canadian Climate Centre for Modelling and Analysis: - Parameterisation of sea-salt optical properties and associated growth for GCMs. Installed in the Canadian GCM model. J. Li, X. Ma, K. von Salzen, and S. Dobbie Parameterization of sea-salt optical properties and physics of the associated radiative forcing Atmos. Chem. Phys., 8, 4787-4798, 2008