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| LEADER |
00000ctm a22000005a 4500 |
| 001 |
in00001307621 |
| 005 |
20220103134658.0 |
| 007 |
cr unu a |
| 008 |
960726s1995 xx ab b 000 0 eng d |
| 035 |
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|9 AHB5844AM
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| 035 |
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|a (OCoLC)35149193
|
| 040 |
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|a TXA
|c TXA
|d UtOrBLW
|
| 049 |
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|a TXAM
|a TXAR
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| 099 |
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|a 1995
|a Thesis
|a S28
|
| 100 |
1 |
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|a Saul, Scott Henry,
|d 1964-
|
| 245 |
1 |
0 |
|a Evolution of vertical drafts and cloud-to-ground lightning within the convective region of a mesoscale convective complex /
|c by Scott Henry Saul.
|
| 264 |
|
1 |
|a [Place of publication not identified] :
|b [publisher not identified] ;
|c 1995.
|
| 300 |
|
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|a xiv, 170 leaves :
|b illustrations, maps ;
|c 28 cm.
|
| 336 |
|
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|a text
|b txt
|2 rdacontent
|
| 337 |
|
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|a computer
|b c
|2 rdamedia
|
| 338 |
|
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|a online resource
|b cr
|2 rdacarrier
|
| 500 |
|
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|a "Major subject: Meteorology".
|
| 500 |
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|a Vita.
|
| 502 |
|
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|b M.S.
|c Texas A&M University
|d 1995.
|
| 504 |
|
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|a Includes bibliographical references.
|
| 520 |
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|a active convection. The relationship of cloud-to-ground (CG)
|
| 520 |
|
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|a analysis times which reached the surface near locations of
|
| 520 |
|
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|a and reflectivity at all levels. CG lightning also occurred
|
| 520 |
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|a and upper-levels but beneath smaller than average
|
| 520 |
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|a beneath greater than average reflectivity gradients at mid
|
| 520 |
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|a comparable to those from a squall line but became much
|
| 520 |
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|a evolution. An analysis of the vertical profiles of the
|
| 520 |
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|a expense of stronger vertical motions. Typically the non-
|
| 520 |
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|a fields for CG lightning. CG lightning occurred beneath
|
| 520 |
|
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|a flash rate. A similar delay was found on the convective
|
| 520 |
|
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|a flow revealed a descending rear-to-front inflow at later
|
| 520 |
|
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|a greater than average vertical velocities at mid-to-upper
|
| 520 |
|
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|a intense updraft cores while cross-sections of storm relative
|
| 520 |
|
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|a lag between the peak convective intensity and the peak CG
|
| 520 |
|
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|a levels and greater than average vertical velocity gradients
|
| 520 |
|
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|a lightning suggested a preferred vertical structure of these
|
| 520 |
|
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|a lightning to the kinematic structure of the MCC was also
|
| 520 |
|
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|a mesoscale convective complex (MCC) was examined over a 100
|
| 520 |
|
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|a minute period during the storm's mature stage and compared to
|
| 520 |
|
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|a Operational and Research Meteorology - Central Phase)
|
| 520 |
|
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|a percentage of weak updrafts and downdrafts grew at the
|
| 520 |
|
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|a PRE-STORM (Preliminary Regional Experiment for Stormscale
|
| 520 |
|
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|a profiles from twenty dual-Doppler analyses indicated
|
| 520 |
|
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|a reflectivity gradients at low-levels due to its avoidance of
|
| 520 |
|
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|a scale for some convective cells, however, other apparently
|
| 520 |
|
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|a sections of both vertical velocity and reflectivity confirmed
|
| 520 |
|
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|a significant differences in convective intensity both
|
| 520 |
|
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|a similar cells had little CG lightning throughout their
|
| 520 |
|
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|a spatially and temporally. The peak magnitudes of the mid-to-
|
| 520 |
|
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|a squall MCC had a much larger percentage of strong downdrafts
|
| 520 |
|
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|a studied. For mesoscale regions there was a 10-20 minute time
|
| 520 |
|
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|a than did the squall line. Horizontal and vertical cross-
|
| 520 |
|
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|a that of a squall line. The area-averaged vertical velocity
|
| 520 |
|
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|a that the MCC was evolving toward a state with fewer and less
|
| 520 |
|
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|a The evolution of the area-averaged vertical velocity within
|
| 520 |
|
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|a the highest reflectivity gradient regions.
|
| 520 |
|
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|a the objectively defined convective region of the 4 June 1985
|
| 520 |
|
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|a upper level area-averaged vertical velocity were initially
|
| 520 |
|
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|a upper levels was consistent with weakening convection as the
|
| 520 |
|
|
|a vertical velocity, reflectivity and their gradients above CG
|
| 520 |
|
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|a weaker. The distribution of vertical velocities at mid-to-
|
| 530 |
|
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|a Also available online.
|
| 530 |
|
|
|a Issued also on microfiche from Lange Micrographics.
|
| 650 |
|
4 |
|a Major meteorology.
|
| 856 |
4 |
1 |
|u https://hdl.handle.net/1969.1/ETD-TAMU-1995-THESIS-S28
|z Link to OAKTrust copy
|t 0
|
| 999 |
|
|
|a MARS
|
| 999 |
f |
f |
|s 35df8599-33b0-3d6e-ba2b-8717c6cbedb3
|i bcb2d531-b67f-354f-badb-c1eadbc838be
|t 0
|
| 952 |
f |
f |
|p noncirc
|a Texas A&M University
|b College Station
|c Cushing Memorial Library & Archives
|s cush tdrm
|d Cushing: Theses & Dissertations Microforms (Does not check out)
|t 0
|e 1995 Thesis S28
|h Other scheme
|i computer -- online resource
|
| 952 |
f |
f |
|a Texas A&M University
|b College Station
|c Electronic Resources
|s www_evans
|d Available Online
|t 0
|e 1995 Thesis S28
|h Other scheme
|
| 998 |
f |
f |
|a 1995 Thesis S28
|t 0
|l Cushing: Theses & Dissertations Microforms (Does not check out)
|
| 998 |
f |
f |
|a 1995 Thesis S28
|t 0
|l Available Online
|