When Saturation Occurs Occurs… … • Heterogeneous Nucleation • Supersaturations very small in atmosphere distrib ibution i sensiitive i to siize • Drop siize di distribution of cloud condensation nuclei 1 2 ICE NUCLEATION PROBLEMATIC Percentage of clouds with ice particle concentrations above detectable level 15 16 16 80 7 1 2 1 1 1 8 23 60 25 40 12 10 14 25 20 33 15 20 0 0 4 3 100 1 1 -5 -10 -15 -20 -25 Cloud top temperature (oC) Image by MIT OpenCourseWare. 3 Precipitation Formation: • Stochastic coalescence (sensitive to drop size distributions) geron-Findeisen Process • Berg • Strongly nonlinear function of cloud water concentration • Time scale of precipitation formation ~1030 minutes 4 Stability No simple criterion based on entropy: T p sd c p ln Rd ln T0 p0 sd , p T p q L s c ln R ln qR ln p T d p vT v 0 0 s, p, qt 5 Virtual Temperature and Density Temperature Assume all condensed water falls at terminal velocity Va Vc Md Mv Mc pV nR *T R *T Va p Md Mv , md mv 6 1 md 1 Md Rd T Va p where here mv Mi i m i M Mv d md 0.622 0 622 Rd R * 7 , md qc a Va Vc Rd T q 1 qt 1 Md Mv Mc p 1 qc c 1 Rd T q 1 qt p Mv Mc Mv qt , q M M Density temperature: q T T 1 qt Rd T p 8 Trick: D fi a saturati Define t tion entropy, t s** : ss* s T , p, qq* s*, p, qt We can add an arbitrary function of qt to s* such that s*', p 9 10 Stability Assessment using Tephigrams: 100 Press sure (mb) 200 300 400 500 600 700 800 900 1000 -40 -30 -20 -10 0 10 Temperature (C) 11 20 30 40 50 Stability Assessment using Tephigrams: Convective Available Potential Energy (CAPE): CAPEi p p e dp pi n p Rd T T d ln p pi p e 12 Other Stability Diagrams: 13 “Air Air--Mass Mass”” Showers: 14 MIT OpenCourseWare http://ocw.mit.edu 12.811 Tropical Meteorology Spring 2011 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms. 15