M-PACE Measurements of IN are consistent with long-lived nature of clouds Binned data from 60 s averages over entire project.

Slides:



Advertisements
Similar presentations
Laboratory Studies of Water Ice Cloud Formation under Martian Conditions Laura T. Iraci, Anthony Colaprete NASA Ames Research Center Bruce Phebus, Brendan.
Advertisements

Boundary Layer Clouds & Sea Spray Steve Siems, Yi (Vivian) Huang, Luke Hande, Mike Manton & Thom Chubb.
Steven Siems 1 and Greg McFarquhar 2 1 Monash University, Melbourne, VIC, Australia 2 University of Illinois, Urbana, IL, USA Steven Siems 1 and Greg McFarquhar.
Cloud Condensation Nuclei Concentrations in the Amazon Basin G P Frank, G Roberts, E Swietlicki, P Artaxo, L Rizzo, P Guyon, O L Mayol-Bracero, A Vestin,
Vivek SantGroup Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed.
CPI International UV/Vis Limb Workshop Bremen, April Development of Generalized Limb Scattering Retrieval Algorithms Jerry Lumpe & Ed Cólon.
Modeling the Growth of Clusters and Aerosols from First Principles: How do We Understand Feedback Systems in a Warming Climate? George C. Shields Department.
Ultrafine Particles and Climate Change Peter J. Adams HDGC Seminar November 5, 2003.
Spectral microphysics in weather forecast models with special emphasis on cloud droplet nucleation Verena Grützun, Oswald Knoth, Martin Simmel, Ralf Wolke.
5. Formation and Growth of Ice Crystals
Effects of size resolved aerosol microphysics on photochemistry and heterogeneous chemistry Gan Luo and Fangqun Yu ASRC, SUNY-Albany
Photo courtesy of Paul Lawson/J.H. Bain An Overview of Cirrus Cloud Thinning and Determining Its Scientific Feasibility David L. Mitchell Desert Research.
Different heterogeneous routes of the formation of atmospheric ice Anatoli Bogdan Institute of Physical Chemistry, University of Innsbruck Austria and.
Bastiaan van Diedenhoven (Columbia University, NASA GISS) Ann Fridlind, Andrew Ackerman & Brian Cairns (NASA GISS) An investigation of ice crystal sizes.
Acknowledgments This research was supported by the DOE Atmospheric Radiation Measurements Program (ARM) and by the PNNL Directed Research and Development.
Chapter 2 Matter and Change Mixtures 2.1 Properties of Matter
February 12, 2004 Recent observational studies on ice nuclei and ice formation in clouds Paul J. DeMott Colorado State University.
Answers. 1 The amount of matter that a material has is its ___. B mass A C D volume density composition.
Motivation and Plans for Natural Source studies in 2014.
June 7, 2004 Laboratory Studies of Ice Initiation by Atmospheric Aerosol Particles Paul J. DeMott With acknowledgment to numerous contributors.
Aerosol Microphysics: Plans for GEOS-CHEM
Horizontal Distribution of Ice and Water in Arctic Stratus Clouds During MPACE Michael Poellot, David Brown – University of North Dakota Greg McFarquhar,
Measurement of free iron content in desert dust : effect on light absorption, size dependence and soil influence S. Lafon, J.-L. Rajot, S. C. Alfaro, A.
LLNL-PRES-XXXXXX This work was performed under the auspices of the U.S. Department of Energy by Lawrence Livermore National Laboratory under contract DE-AC52-07NA27344.
Improving Black Carbon (BC) Aging in GEOS-Chem Based on Aerosol Microphysics: Constraints from HIPPO Observations Cenlin He Advisers: Qinbin Li, Kuo-Nan.
11 The potential impact of mineral dust on cirrus (and other) cloud formation: a trajectory modeling perspective Aldona Wiącek * and Thomas Peter ETH,
Types of Mixtures w Variable combination of 2 or more pure w substances. Heterogeneous Homogeneous.
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.
What is matter? What are the states of matter? What changes occur to matter? What are mixtures and the different types? How do we separate mixtures? Matter,
GISS GCM Developmental Efforts for NASA MAP Program Surabi Menon, Igor Sednev (LBNL) and Dorothy Koch, Susanne Bauer (NASA GISS/Columbia University) and.
Morrison/Gettelman/GhanAMWG January 2007 Two-moment Stratiform Cloud Microphysics & Cloud-aerosol Interactions in CAM H. Morrison, A. Gettelman (NCAR),
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.
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.
Influences of In-cloud Scavenging and Cloud Processing on Aerosol Concentrations in ECHAM5-HAM Betty Croft - Dalhousie University, Halifax, Canada Ulrike.
NASA CMAI WorkshopApril 20-21, 2006 Modeling Studies of Aerosol-Cold Cloud Interactions Sonia M. Kreidenweis and Paul J. DeMott Department of Atmospheric.
Ice Crystal Parameterizations in Arctic Cirrus – Towards a Better Representation in Global Climate Models and Aircraft Icing Potential Studies Victoria.
In situ observations of water vapor and cirrus IWC in the Pacific TTL during ATTREX Troy Thornberry, Drew Rollins, Ru-Shan Gao, David Fahey Paul Bui, Sarah.
Potential alteration of ice clouds by aircraft soot Joyce E. Penner and Xiaohong Liu Department of Atmospheric, Oceanic and Space Sciences University of.
Study Flow Diagram Holvoet P, et al. JAMA 2008;299: The Figure shows the selection of 1889 participants who did not have metabolic syndrome at year.
Radiative Influences on Glaciation Time-Scales in Mixed-Phase Clouds Zachary Lebo, Nathanial Johnson, and Jerry Harrington Penn State University Acknowledgements:
Guy Cascella, in association with MPO531, presents: Featuring: African dust aerosols as atmospheric nuclei, DeMott et al, 2003 Chemical characteristics.
October 27, 2015 Objective: I will be able to describe how water is recycled through the environment in a process called the water cycle. Entry Task: Make.
Horizontal Variability In Microphysical Properties of Mixed-Phase Arctic Clouds David Brown, Michael Poellot – University of North Dakota Clouds are strong.
COSMO General Meeting, WG3-Session, 7 Sep Cloud microphysics in the COSMO model: New parameterizations of ice nucleation and melting of snow.
ICE - Laboratory experiment goals Basic scientific understanding Check performance of airborne instruments Develop new measurement techniques & combining.
Application of Ice Microphysics to CAM Xiaohong Liu, S. J. Ghan (Pacific Northwest National Laboratory) M. Wang, J. E. Penner (University of Michigan)
Cloudnet Workshop April 2003 A.Tompkins 1 Changes to the ECMWF cloud scheme  Recent package of changes for 25r3:  COMPLETE REWRITE OF NUMERICS FOR CLOUD.
Production of Ice in Tropospheric Clouds by Will Cantrell and Andrew Heymsfield Presentation by: Emily Riley 27 February 2007.
Update on progress with the implementation of a new two-moment microphysics scheme: Model description and single-column tests Hugh Morrison, Andrew Gettelman,
1)Consideration of fractional cloud coverage Ferrier microphysics scheme is designed for use in high- resolution mesoscale model and do not consider partial.
Development of cloud resolving model with microphysical bin model and parameterizations to predict the initial cloud droplet size distribution KUBA, Naomi.
October 22, 2015 Objective: I will be able to relate the phase changes of water to the kinetic molecular theory of matter. Entry Task: Read “Boiling Oil”
The Regional Conference on Dust and Dust Storms November, Sheraton, Kuwait World Meteorological Organization Working together in weather, climate.
COPE PRESENTATION Process Modeling and Ice Nuclei.
Homogeneous nucleation: freezing of supercooled water Exponential dependence arises from energy term T dependence from this term.
B3. Microphysical Processes
Environmental Physics Laboratory, Institute of Physics Belgrade
Formation of cirrus cloud by glassy aerosols
Review for Exam 2 Fall 2011 Topics on exam: Class Lectures:
H. Morrison, A. Gettelman (NCAR) , S. Ghan (PNL)
VI-ACI kickoff meeting, Karlsruhe, May 14/15, 2007.
By Gourihar Kulkarni Steven Dobbie Mike Smith Jim McQuaid
Microphysics of Cold Clouds
ATOC 4720 class19 Thunderstorms 1. Growth of clouds droplets in
Freezing Pathways Homogenous  Deposition  Contact  Condensation 
GCM activities in Ulrike Lohmann’s group
About Tatu’s recent work
Chapter 2 Review.
Chapter 2 Review.
Presentation transcript:

M-PACE Measurements of IN are consistent with long-lived nature of clouds Binned data from 60 s averages over entire project

[IN] variability and dependence on supersaturation in mixed-phase regime measured at altitude for different locales Relevance: Mixed phase clouds

Ice nucleation by coated dusts amenable to parameteric/threotical treatments Classical theory applied to iron oxide/H 2 SO 4 /H 2 O freezing  a w(het) <  a w(hom) Exploited for parameterization by Kärcher and Lohmann (2003, JGR) Water activity based freezing theory applied to heterogeneous freezing Archuleta et al. (2005) Adapted from Zuberi et al. (2002, GRL) Archuleta et al. (2005)

Nucleation rate for iron oxide particles (sizes to 200 nm)

Laboratory natural dust sample comparisions – size and generation method matter Note similarity of behavior to large mineral particles studied by Roberts and Hallett (1968, QJRMS)