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observational data

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poster Wednesday] Stronger easterlies, deeper and moister layers, more rain ... The environment of precipitating shallow convection' (poster Wednesday) ... – PowerPoint PPT presentation

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Title: observational data


1
The chances of getting wet Louise Nuijens
UCLA - Dept. Atmospheric Oceanic
Sciences GCSS Toulouse - June 2, 2008
2
Lots of rain
3
Motivation
What regulates the large variability in shallow
precipitation within the undisturbed trades?
4
Ideas
  • random?
  • deeper clouds, more clouds, more rain?
  • Austin, 1948 - Stevens and Seifert, 2007
  • Variability in meteorology?
  • stability
  • humidity (deep convection strong relation
    column water vapor and precipitation)
  • Bretherton et al, 2004 - Holloway and
    Neelin, 2008
  • Variability in the aerosol?
  • more CCN, less rain? Colon-Robles
    et al, 2006 - Hudson and Mishra, 2006
  • (more cloud?)

5
Data and methods
  • Data
  • 3300 horizontal radar scans (SPolKa)
  • 200 soundings from land (SPNT), ship (RVSJ),
    aircraft (C130)
  • lidar data from C130 circles flown at 4.5 km
  • Method
  • composites (either 2, 3 or 6) of data
  • for periods of little, moderate and widespread
  • precipitation, based on six hour mean echo
  • fractions of NE radar domain.
  • excluding days with heavy precipitation
  • using echo fraction as a proxy for rainfall

6
Deeper and more clouds more rain
Trivej and Stevens The power law and echo size
distribution', poster Wednesday
7
Stronger easterlies, deeper and moister layers,
more rain


8
Relations between winds, precipitation and
humidity

9
But higher winds is more aerosol?

CCN / MD data from Hudson and Mishra, 2007
10
Vertical distribution of echo fraction for
flights with low vs high aerosol
11
Stronger easterlies, higher humidity?
12
Summary
  • Precipitation varies most strongly with
    humidity and the strength of the easterlies
  • Deeper clouds and greater inversion heights at
    times of more rain
  • Between periods of little and moderate precip,
    moistening predominantly
  • forced from bottom shifting to the top
    between periods of moderate and
  • widespread precip
  • and suggest that subtle variations in zonal
    wind speeds (and surface
  • evaporation) and subsidence, even within this
    meteorological regime, can
  • regulate humidity, hence precipitation
  • Variability in the aerosol likely plays a minor
    role
  • Nuijens, Stevens and Siebesma
  • ' The environment of precipitating shallow
    convection' (poster Wednesday)
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