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Hydrometeors Injected into the Large-scale Environment by Tropical Cloud Systems Robert A. Houze & Courtney Schumacher Co-PIs ARM Science Team Meeting,

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Presentation on theme: "Hydrometeors Injected into the Large-scale Environment by Tropical Cloud Systems Robert A. Houze & Courtney Schumacher Co-PIs ARM Science Team Meeting,"— Presentation transcript:

1 Hydrometeors Injected into the Large-scale Environment by Tropical Cloud Systems Robert A. Houze & Courtney Schumacher Co-PIs ARM Science Team Meeting, Albuquerque, New Mexico, 27 March 2006

2 Tropical MCSs inject lots of hydrometeors into upper troposphere Idealized life cycle of tropical MCS as proposed by Houze 1982

3 Think of the following schematic as a composite of the water budget of an MCS over its whole life cycle After Houze et al. (1980)

4 Stratiform water budget equation

5 Cloud radar  E se Precip radar  R s Doppler  E sd, C su, C T Measurements

6 In TWP-ICE we are subdividing the anvil into mixed and ice anvils

7 13˚ S 11˚ S 12˚ S 130˚E132˚E131˚E 6060 5353 4646 3939 3232 2525 1818 1 4 dB Z 20 January 2006 0000UTC 6 km 13˚ S 11˚ S 12˚ S 130˚E132˚E 131˚E 6060 5353 4646 3939 3232 2525 1818 1 4 dB Z 20 January 2006 0900UTC 6 km 13˚ S 11˚ S 12˚ S 130˚E132˚E 131˚E 6060 53 46 39 32 25 18 11 4 dBZ 20 January 2006 1800UTC 6 km Example from TWP-ICE dBZ 20 2200 19Jan06 0000 20Jan06 0200 20Jan06 0400 20Jan06 0600 20Jan06 0800 20Jan06 1000 20Jan06 1200 20Jan06 1400 20Jan06 1600 20Jan06 1800 20Jan06 2000 20Jan06 28 21 14 7 0 -7 -14 -21 -28 ATTENUATED Height (km) 4 8 12 16 0 Cloud Radar Precipitation Radar

8 TWP-ICE Precipitation Radar Rain Rate (~20 % stratiform) TWP-ICE Cloud Radar Anvil Frequency Longer-term records of the water budget parameters also are being derived. Figures here are for duration of TWP-ICE. This will also be done for a longer-term climatology. We will use cloud & precipitation radars permanently located at Darwin.

9 Using the empirically derived water budget parameters b and  s, the stratiform regions’ anvil mass is proportional to the stratiform rain E se =(bR s )/  s 200 hPa streamfunction response to CRF assumed proportional to TRMM rain by Schumacher et al. (2004) 400 hPa K/day

10 Summary Water budget relationships will be used to investigate the magnitude & mechanisms of anvil generation by convective systems Cloud & Precipitation Radar will be used to estimate terms in the water budgets, & water budget terms will be checked for internal consistency The TWP-ICE dataset is being used to estimate the water budget terms for some representative cases, & for long-term dataset at Darwin Will develop formulas for parameterizing the anvil mass in terms of satellite observed rainfall.

11 Thank you!


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