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NAME:IMK Kalender / IMK Calendar
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DTSTAMP:20261104T222321Z
SUMMARY:On the scale dependency and generation of longwave atmospheric
 cloud-radiative effects


X-ALT-DESC;FMTTYPE=text/html:<!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 
 3.2//EN"><HTML><HEAD><TITLE></TITLE></HEAD><BODY>On the scale dependency 
 and generation of longwave atmospheric cloud-radiative 
 effects<br><br><br>KIT Campus Süd, Gebäude 30.22, 
 Otto-Lehmann-Hörsaal<br><br><p>Longwave atmospheric cloud-radiative 
 effect (LW ACRE) is important in supporting a variety of spatially 
 organized moist systems in tropical weather and climate, from tropical 
 cyclones, the Madden-Julian oscillation (MJO), to Walker circulation. 
 Our works aim to understand the fundamental properties and the processes 
 that generate the feedback between LW ACRE and tropical precipitating 
 convection. I will discuss two major findings. (1) We explain why LW 
 ACRE only supports larger-scale circulations, as in the MJO but not in 
 mesoscale convective systems (MCSs), by studying a field campaign MCS 
 case. (2) Why does such scale dependency exist? We propose a minimal 
 conceptual recipe to quantitatively describe the scale dependency of 
 LW-convection feedback by simply assuming that anvil clouds, which 
 primarily generate LW ACRE, act as long-term memory of precipitation. 
 The scale dependency of LW-convection feedback is, thus, a natural 
 emerging property of longer memory of anvil clouds than precipitation. 
 Finally, I will discuss how this conceptual model may provide 
 information of how anvil LW ACRE is generated in tropical convective 
 systems.</p><br></BODY></HTML>
DESCRIPTION: On the scale dependency and generation of longwave
 atmospheric cloud-radiative effects\n\n\nKIT Campus Süd, Gebäude
 30.22, Otto-Lehmann-Hörsaal\n\n<p>Longwave atmospheric cloud-radiative
 effect (LW ACRE) is important in supporting a variety of spatially
 organized moist systems in tropical weather and climate, from tropical
 cyclones, the Madden-Julian oscillation (MJO), to Walker circulation.
 Our works aim to understand the fundamental properties and the processes
 that generate the feedback between LW ACRE and tropical precipitating
 convection. I will discuss two major findings. (1) We explain why LW
 ACRE only supports larger-scale circulations, as in the MJO but not in
 mesoscale convective systems (MCSs), by studying a field campaign MCS
 case. (2) Why does such scale dependency exist? We propose a minimal
 conceptual recipe to quantitatively describe the scale dependency of
 LW-convection feedback by simply assuming that anvil clouds, which
 primarily generate LW ACRE, act as long-term memory of precipitation.
 The scale dependency of LW-convection feedback is, thus, a natural
 emerging property of longer memory of anvil clouds than precipitation.
 Finally, I will discuss how this conceptual model may provide
 information of how anvil LW ACRE is generated in tropical convective
 systems.</p>\n
DTSTART;TZID=Europe/Berlin:20270112T154500
DTEND;TZID=Europe/Berlin:20270112T164500
LOCATION:KIT Campus Süd, Gebäude 30.22, Otto-Lehmann-Hörsaal
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