ABSTRACT - DRUM - University of Maryland

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Zhou X. L., M. A. Geller, and M. H. Zhang, Cooling trend <strong>of</strong> the tropical cold point tropopause temperatures and its implications, J. Geophys. Res., 106 (D2), 1511-1522, 2001 Zőger, M., A. Engel, D. S. McKenna, C. Schiller, U. Schmidt, and T. Woyke, Balloonborne in situ measurements <strong>of</strong> stratospheric H 2O , J.Geophys.Res., 104 (D1), 1817- 1825, 1999 83
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the time evolution of local convect
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ACKNOWLEDGMENTS I foremost would li
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2.3.4 Regional distribution .......
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LIST OF FIGURES 1.1 Convective impa
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3.6 A schematic of possible errors
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This dissertation includes two stud
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forces from the stratosphere by wav
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Figure 1.1 describes the impact of
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Detrained air from convective cloud
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water vapor, as well as the chemica
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vapor mixing ratio with altitude in
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Instrument [H 2 O] e (ppmv) Period
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that recent lidar images of thin ci
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Troposphere Exchange Project (STEP/
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1. Observation of tropopause coolin
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are locally associated with cold an
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channels of four weather satellites
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Figure 2.1 An example of convective
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Temperature (K) Figure 2.3 Same wit
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temperature profile. The anomalies
Page 43 and 44: Figure 2.4 Cooling rate calculation
Page 45 and 46: Figure 2.5 Sensitivity tests in (a)
Page 47 and 48: Potential temperature (K) Figure 2.
Page 49 and 50: 2.4.2 Cloud-top radiative cooling I
Page 51 and 52: the daytime and nighttime convectiv
Page 53 and 54: which implies approximately 35% of
Page 55 and 56: Chapter 3. A study of tropical deep
Page 57 and 58: not quantitatively indicate the ext
Page 59 and 60: Figure 3.1 A cartoon of overshootin
Page 61 and 62: there is, as expected, a general sy
Page 63 and 64: Figure 3.3 Geophysical distribution
Page 65 and 66: Figure 3. 5 Mean of scatter plots i
Page 67 and 68: horizontal error bars in Fig. 3.5 a
Page 69 and 70: example, if we use A = 3 km, s = 1,
Page 71 and 72: Figure 3. 7 A moist adiabatic model
Page 73 and 74: Figure 3. 8 Total heights of the ov
Page 75 and 76: Chapter 4. Summary and Conclusions
Page 77 and 78: In order to see how fast this conve
Page 79 and 80: is estimated from visible and near-
Page 81 and 82: -7 K/day. This cooling speed is bey
Page 83 and 84: References Abbas, M. M., H. A. Mich
Page 85 and 86: Dessler, A. E. and H. Kim, Determin
Page 87 and 88: Hurst, D. F., G. S. Dutton, P. A. R
Page 89 and 90: Kummerow, C., W. Barnes, T. Kozu, J
Page 91 and 92: Randel, W. J., F. Wu, and W. Rivera
Page 93: Stenke A. and V. Grewe, Impact of d
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