Microphysics Measurements During CLACE 2014 G.J. Lloyd 1, R. Farrington, P.Connolly 1 T.W. Choularton 1, M. Gallagher 1 and K. N. Bower 1 1 Centre for.

Slides:



Advertisements
Similar presentations
Weather Vocabulary Words Meteorologist Weather Temperature Wind Front Anemometer Precipitation Cloud coverage Weather Map.
Advertisements

Fine-Scale Variations in Aerosol Transport within a Street Canyon – a Pilot Field Study I.D. Longley, M.W. Gallagher, M. Flynn, J.R. Dorsey, P.I. Williams.
World Meteorological Organization Working together in weather, climate and water Snowfall Measurement Challenges WMO SPICE Solid Precipitation Intercomparison.
Application of Cloudnet data in the validation of SCIAMACHY cloud height products Ping Wang Piet Stammes KNMI, De Bilt, The Netherlands CESAR Science day,
Jeopardy MatterClouds Water Cycle Weather Maps Q $100 Q $200 Q $300 Q $400 Q $500 Q $100 Q $200 Q $300 Q $400 Q $500 Final Jeopardy.
Notes on Weather A.Weather is the short term condition of the atmosphere over a small area. B.Weather is described by its conditions, or variables that.
Electroscavenging of Condensation and Ice- Forming Nuclei Brian A. Tinsley University of Texas at Dallas WMO Cloud Modeling Workshop,
Hallet-Mossop Process as a Mechanism for Ice Multiplication Steven Brown Atmospheric Sciences 5/16/2011.
By : Kerwyn Texeira. Outline Definitions Introduction Model Description Model Evaluation The effect of dust nuclei on cloud coverage Conclusion Questions.
K M Beswick 1, M W Gallagher 1, D Baumgardner 2, P Nedelec 3, S Devereau 4, S Lance 5 Contact Information 1 SEAES, University of Manchester, Oxford Road,
Applications of satellite measurements on dust-cloud-precipitation interactions over Asia arid/semi-arid region Jianping Huang Key Laboratory for Semi-Arid.
Microstructure of Israeli Clouds and their Suitability for Seeding Eyal Freud and Daniel Rosenfeld יום עיון מחקרי רשות המים, 21 ביוני 2011.
Page 1© Crown copyright The Facility for Airborne Atmospheric Measurements (FAAM) BAe-146 Steve Abel First VOCALS Regional Experiment (REx) Preparatory.
Weather Cathcart 6 th grade science. What is weather? Weather is the condition of the atmosphere at a certain time and place.
PARTICLE FLUXES MEASURED BY EDDY COVARIANCE ABOVE AND WITHIN A DOWNTOWN URBAN CANOPY I.D. Longley, M.W. Gallagher School of Earth, Atmospheric & Environmental.
Anthropogenic Aerosol – A Cause Of The Weekend Effect? A significant weekly cycle has been found in diurnal temperature range (DTR). A candidate for causing.
ENVI3410 : Lecture 8 Ken Carslaw
Multiwavelength aerosol lidar and vertical-wind lidar observations during COPS Dietrich Althausen, Detlef Müller, Ronny Engelmann, Matthias Tesche, Patric.
Observational approaches to understanding cloud microphysics.
D. Waddicor, G. Vaughan, K. Bower, T. Choularton, H. Coe, M. Flynn, M. Gallagher, P. Williams Aerosol observations and growth rates in the TTL.
Daniel Grosvenor, Thomas Choularton, Martin Gallagher (University of Manchester, UK); Thomas Lachlan Cope and John King (British Antarctic Survey). Daniel.
By Kristie Ewing ECE 8814/03 Georgia Performance Standards What is Weather? Who Studies Weather? Weather Instruments –Observation –Thermometer –Wind.
Cloud Microphysics SOEE3410 : Lecture 4 Ken Carslaw Lecture 2 of a series of 5 on clouds and climate Properties and distribution of clouds Cloud microphysics.
Weather!.
Remote-sensing of the environment (RSE) ATMOS Analysis of the Composition of Clouds with Extended Polarization Techniques L. Pfitzenmaier, H. Russchenbergs.
Acknowledgments This research was supported by the DOE Atmospheric Radiation Measurements Program (ARM) and by the PNNL Directed Research and Development.
TEST Review CH 11 ATMOSPHERE p Earth Science Review Sheet 1 st day of Semester.
ISCCP at 30. Influence of aerosols on mesoscale convective systems inferred from ISCCP and A-Train datasets Rong Fu & Sudip Chakraborty Jackson School.
Julie Haggerty National Center for Atmospheric Research Friends and Partners of Aviation Weather October July 2014.
Wednesday, 9/16/091 ATMO Class #8 Wednesday, September 16, 2009 Chapter 4, Water in the atmosphere.
Arctic Clouds: A missing puzzle piece. Ideas we will cover How thick is the atmosphere? The climate system is COMPLICATED Greenhouse gases warm the planet.
Modern Era Retrospective-analysis for Research and Applications: Introduction to NASA’s Modern Era Retrospective-analysis for Research and Applications:
Airborne survey of dust & clouds V. Ramanathan and Joachim Koettner –NCAR visit –last April, CIFEX (Cloud Indirect Effects Experiment) –expressed interest.
Morrison/Gettelman/GhanAMWG January 2007 Two-moment Stratiform Cloud Microphysics & Cloud-aerosol Interactions in CAM H. Morrison, A. Gettelman (NCAR),
CLOUDS. What are clouds?
Weather How Cold Will it be Tomorrow? Heat Transfer As temperature rises, the energy within a molecule also increases Radiation-direct transfer of heat.
Essential Question How do Meteorologist Predict Weather?
Testing LW fingerprinting with simulated spectra using MERRA Seiji Kato 1, Fred G. Rose 2, Xu Liu 1, Martin Mlynczak 1, and Bruce A. Wielicki 1 1 NASA.
Regional Modeling of Antarctic Clouds Keith M. Hines 1 and David H. Bromwich 1,2 1 Polar Meteorology Group Byrd Polar Research Center The Ohio State University.
Antarctic Clouds Tom Lachlan-Cope John King, Amélie Kirchgaessner.
Potential of the ATHAM model for use in air traffic safety Gerald GJ Ernst Geological Institute, University of Ghent, Gent, Belgium Christiane Textor Lab.
Distribution of Liquid Water in Orographic Mixed-Phase Clouds Diana Thatcher Mentor: Linnea Avallone LASP REU 2011.
A study of ice formation by primary nucleation and ice multiplication in shallow precipitating embedded convection T. Choularton 1, I. Crawford 1, C. Dearden.
MODIS Level 3: Future Issues and Considerations Brent Maddux MODIS Level 3: Future Issues and Considerations Brent Maddux Cloud Fraction Mean.
The Water Cycle…. The story of each raindrop.. The Sea  The Earth has massive oceans that store the majority of our water  At sea, the sun heats the.
Types of Precipitation Precipitation comes in two forms Precipitation comes in two forms Liquid – rain, drizzle Liquid – rain, drizzle Solid - freezing.
Dr David Healy Professor John Sodeau Dr Stig Hellebust Dr Daniela Iacopino Professor Paul Kaye Dr Warren Stanley EPA (Ireland) for funding (STRIVE-CCRP)
Global Modeling Status Thomas Lachlan-Cope 1 and Keith M. Hines 2 1 British Antarctic Survey Cambridge, UK 2 Polar Meteorology Group Byrd Polar Research.
INUPIAQ/CLACE 2014 University of Manchester Data availability.
Daniel Grosvenor, Thomas Choularton, Martin Gallagher (University of Manchester, UK); Thomas Lachlan Cope and John King (British Antarctic Survey). Daniel.
Relationship Between Cloud Droplet Effective Radius and Cloud Top Height for Deep Convective Clouds in CloudSat Data Product Satoshi Suzuki, Shinta Seto,
Describes the condition of the atmosphere such as temperature, cloud cover, wind speed, and rainfall.
DO Now 1._____ layer that satellites orbit (atm layers) 2._____ most abundant gas in the atmosphere (atmosphere) 3._____changes from water vapor to a liquid.
Clouds, Rain Processes and Biosphere Interaction in LBA Maria A. F. Silva Dias Department of Atmospheric Sciences University of São Paulo Brazil.
Update on the 2-moment stratiform cloud microphysics scheme in CAM Hugh Morrison and Andrew Gettelman National Center for Atmospheric Research CCSM Atmospheric.
Aerosol 1 st indirect forcing in the coupled CAM-IMPACT model: effects from primary-emitted particulate sulfate and boundary layer nucleation Minghuai.
Global Warming The heat is on!. What do you know about global warming? Did you know: Did you know: –the earth on average has warmed up? –some places have.
COPE PRESENTATION Process Modeling and Ice Nuclei.
Water Cycle, Cloud Formation, and Severe Weather.
How Solar Technologies can benefit from the Copernicus Project Nur Energie November 2015.
JFJ 2013 Aim: to identify the best upwind site for the 2014 campaign P. Connolly Centre for Atmospheric Science.
Microphysics observations from MICRO-SCOPE J. Crosier, Z. Liu, J. Taylor, K. Bower, T. Choularton University of Manchester COPE meeting - Leeds - April.
Current State of Processing of the PECAN Microphysics Dataset
A model of sea salt aerosol for Cape Grim Preliminary investigations
Rain Snow Hailstones Ice Rime Dew  All types of moisture reaching the surface of earth from atmosphere  Precipitation is the basic input to the hydrology.
Water & Precipitation Notes
The role of weather conditions on PM2.5 concentrations in Beijing
Turbulence-induced broadening of cloud-droplet size distributions: Implications for aerosol effects on climate Tuesday, April 25, :00-12:00 Noon.
The story of each raindrop.
Unit: Water and the Atmosphere Lesson #3: Precipitation Essential Questions: 1.) What are the common types of precipitation? 2.) What are the causes and.
Presentation transcript:

Microphysics Measurements During CLACE 2014 G.J. Lloyd 1, R. Farrington, P.Connolly 1 T.W. Choularton 1, M. Gallagher 1 and K. N. Bower 1 1 Centre for Atmospheric Science, SEAES, University of Manchester, M13 9PL, Manchester, U.K.

Priority Cases 30 Jan – 2 Feb Saharan Dust Event 8 – 9 Feb Liquid/Ice transitions 18 – 19 Feb Saharan Dust 11 – 12 Feb Inc/Dec Ice Fractions 14 Feb Further ice/liq fluctuations

Aims Identify periods of changing microphysics – Short term fluctuations (seconds) – Larger temporal scale changes (hours) Are these changes associated with something? – Temperature – Wind – Aerosol

Instrumentation 3VCPI (2DS) Measurement of cloud particles 10 < d p < 1280 µm Discrimination of lce/Liquid CDP Measurement of liquid droplets 2 < d p < 50 µm WIBS4 Aerosol Measurements

11 – 12 Feb

A B

A 1.28mm

B

11 – 12 Feb

30 Jan – 2 Feb

A B

A 1.28mm

B

30 Jan – 2 Feb

2D-S Irregular Concentration vs WIBS4 FL Concentration

30 Jan – 2 Feb

Swift Transitions – 8 Feb

1.28mm

18 – 19 Feb

Wind Blown Snow??

Wind Blown Snow

Conclusions Transitions between liquid and glaciated conditions frequent Significant ‘Saharan’ dust events identified Some signs of a correlation between inc ice and inc fluorescent aerosol? Wind blown snow may not contribute significantly

Feedback: Privacy Policy Feedback
Do Not Sell My Personal Information
About project: SlidePlayer Terms of Service

© 2024 SlidePlayer.com Inc. All rights reserved.