paul lawson and brad baker (spec) eric jensen (nasa arc), david mitchell (dri)

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Paul Lawson and Brad Baker (SPEC) Eric Jensen (NASA ARC), David Mitchell (Dri) Microphysical and Radiative Microphysical and Radiative Properties of Tropical Clouds Properties of Tropical Clouds R R esults from TC4 and NAMMA esults from TC4 and NAMMA

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Microphysical and Radiative Properties of Tropical Clouds R esults from TC4 and NAMMA. Paul Lawson and Brad Baker (SPEC) Eric Jensen (NASA ARC), David Mitchell (Dri). Anvil and Turrets on 7/24. Aged Anvil Cirrus on 8/8. In Situ Cirrus on 7/22. - PowerPoint PPT Presentation

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Page 1: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Paul Lawson and Brad Baker (SPEC) Eric Jensen (NASA ARC), David Mitchell (Dri)

Microphysical and Radiative Microphysical and Radiative Properties of Tropical Clouds Properties of Tropical Clouds RResults esults

from TC4 and NAMMAfrom TC4 and NAMMA

Page 2: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Anvil and Turrets on 7/24 Aged Anvil Cirrus on 8/8

In Situ Cirrus on 7/22

Page 3: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)
Page 4: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)
Page 5: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)
Page 6: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)
Page 7: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Decrease in Number Concentration, Extinction and Mass

Across a TC4 Anvil from DC-8 In Situ Data at FL370 on 24 July 2008

Page 8: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Jensen et al. (2009)

Page 9: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)
Page 10: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)
Page 11: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

TWP-ICE

~ 100 km Downwind ~ 300 km Downwind

Page 12: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Examples of Crystal Chains Formed in Continental Anvils

With High Electric Fields (Connolly et al. 2005 - QJRMS)

Page 13: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Comparison of Cloud Radiative Heating ProfilesComparison of Cloud Radiative Heating Profiles

Mitchell MADA Code used to Compute Optical Properties (SSA, g(SSA, g, , ext) from 2D-S Area and Mass PSD’s

Optical Properties fed into Toon et al. (1989) Two-Stream Radiative Transfer Code to Compute Heating Rates.

Page 14: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Comparison of Cloud Radiative Heating ProfilesComparison of Cloud Radiative Heating Profiles

Page 15: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Comparison of Cloud Radiative Heating ProfilesComparison of Cloud Radiative Heating Profiles

Page 16: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Comparison of Cloud Radiative Heating ProfilesComparison of Cloud Radiative Heating Profiles

Page 17: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Comparison of Cloud Radiative Heating ProfilesComparison of Cloud Radiative Heating Profiles

Page 18: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

Comparison of Cloud Radiative Heating ProfilesComparison of Cloud Radiative Heating Profiles

Page 19: Paul Lawson and Brad Baker (SPEC)  Eric Jensen (NASA ARC), David Mitchell (Dri)

CVI and 2D-S IWC Agree to Within About 20% in the mean. Average Microphysical Properties are Similar from one

Tropical Maritime Region (TC4) to Another (NAMMA) Significant Microphysical Variability (i.e., Particle

Concentration, ext, IWC, Particle Shape) Exists Within a Region on scales from Tens to Thousands of Kilometers, however, Particles from about 100 to 400 m Dominate Extinction and IWC in all Cloud Types.

Two-Stream Radiative Transfer Model (Toon 1989) gives Cloud Heating Rates using Actual In Situ Measurements.

SummarySummaryConc.

cc-1

extKm-1

IWC g m-3

0.1 0.5 0.01 0.5

0.1 1 0.03 2

0.5 15 0.5 25

5 50 1.5 500

In Situ Cirrus: Aged Anvil Cirrus: Fresh Anvil Cirrus: Convective Turrets: