Difference between revisions of "Presentations and Posters"

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==Presentations==
 
==Presentations==
   
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* {{pdf|UKCA_aerosol_BryanLawrence_Oct2012_final.pdf‎| UKCA aerosol: current status, science and future development plans (Sep 2012)}} (G. Mann)
 
* {{pdf|Mann_NCASClimateSeminar_Reading_May11.pdf|State-of-the-science in aerosol-climate models;Current and future science with UKCA aerosol (May 2011)}} (G. Mann)
 
* {{pdf|Mann_NCASClimateSeminar_Reading_May11.pdf|State-of-the-science in aerosol-climate models;Current and future science with UKCA aerosol (May 2011)}} (G. Mann)
 
* {{pdf|PB_MIPAS_DUM.pdf|Confronting UKCA with MIPAS Observations}} (P. Braesicke)
 
* {{pdf|PB_MIPAS_DUM.pdf|Confronting UKCA with MIPAS Observations}} (P. Braesicke)
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==Posters==
 
==Posters==
   
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* {{pdf|DhomseEGU2013.pdf|Whole-atmosphere aerosol microphysics simulations of the Mount Pinatubo eruption: an evaluation (Apr 2013, EGU conference)}} (S. Dhomse)
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* {{pdf|Mann_ICAS_AwayDay_UKCAaerosol_Oct2012.pdf‎|Simulated aerosol properties in HadGEM-UKCA, comparison to TOMCAT-GLOMAPmode and a range of benchmark observational datasets (Oct 2012)}} (G. Mann).
 
* {{pdf|SPARC08_Age_PB.pdf|Zonal Asymmetries in Age-of-air and their Relevance for Transport into the Subtropical Lowermost Stratosphere}} (P. Braesicke)
 
* {{pdf|SPARC08_Age_PB.pdf|Zonal Asymmetries in Age-of-air and their Relevance for Transport into the Subtropical Lowermost Stratosphere}} (P. Braesicke)
 
* {{pdf|SPARC08_WWind_PB.pdf|The Role of Tropical Vertical Velocities in Determining Tracer Gradients in the Upper Troposphere and Lower Stratosphere}} (P. Braesicke)
 
* {{pdf|SPARC08_WWind_PB.pdf|The Role of Tropical Vertical Velocities in Determining Tracer Gradients in the Upper Troposphere and Lower Stratosphere}} (P. Braesicke)

Latest revision as of 17:38, 2 December 2013

Presentations

Posters

UKCA Launch Meeting Presentations