| Tag |
First Indicator |
Second Indicator |
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| LEADER |
00000ctm a22000005a 4500 |
| 001 |
in00001307613 |
| 005 |
20220103114429.0 |
| 007 |
cr unu a |
| 008 |
960726s1995 xx a b 000 0 eng d |
| 035 |
|
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|9 AHB5836AM
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| 035 |
|
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|a (OCoLC)35149044
|
| 040 |
|
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|a TXA
|c TXA
|d UtOrBLW
|
| 049 |
|
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|a TXAM
|a TXAR
|
| 099 |
|
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|a 1995
|a Thesis
|a R576
|
| 100 |
1 |
|
|a Ritz, Richard Lee,
|d 1960-
|
| 245 |
1 |
0 |
|a Dynamical interactions between a mid-tropospheric closed cyclone, a low-level jet, and cyclogenesis /
|c by Richard Lee Ritz.
|
| 264 |
|
1 |
|a [Place of publication not identified] :
|b [publisher not identified] ;
|c 1995.
|
| 300 |
|
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|a xi, 99 leaves :
|b illustrations, maps ;
|c 28 cm.
|
| 336 |
|
|
|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 and the LLJ. A statistical analysis of the Eta Model results
|
| 520 |
|
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|a cyclone was related to the interactions of the upper- and
|
| 520 |
|
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|a descent of potential vorticity from the stratosphere along an
|
| 520 |
|
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|a development of a lower-level cyclone. A LLJ developed over
|
| 520 |
|
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|a During this episode, a trough developed in the lee of the
|
| 520 |
|
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|a established by 1200 UTC 16 October 1994, as stratospheric
|
| 520 |
|
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|a followed the descent of high potential vorticity air into the
|
| 520 |
|
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|a high spatial and temporal resolution of the Eta Model made it
|
| 520 |
|
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|a indicated that the model provided an accurate representation
|
| 520 |
|
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|a interacted with the low-level baroclinic zone initiating the
|
| 520 |
|
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|a isolated in the base of the trough. The upper-level cyclone
|
| 520 |
|
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|a large-scale forcing. A schematic diagram was constructed
|
| 520 |
|
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|a LLJ and the ULJ. The rapid development of the surface
|
| 520 |
|
|
|a lower-level cyclonic systems and the LLJ and ULJ.
|
| 520 |
|
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|a middle troposphere with the cyclone cutting off from the
|
| 520 |
|
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|a movement of the upper-level low into the northern Great
|
| 520 |
|
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|a October 1994. Formation of an upper-level low followed
|
| 520 |
|
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|a of a cutoff cyclone, a low-level jet (LLJ), cyclogenesis, and
|
| 520 |
|
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|a of the atmospheric situation. The formation of a cutoff low
|
| 520 |
|
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|a Output from the Eta Model was used to examine the development
|
| 520 |
|
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|a Plains. To study this event, the Eta Model was chosen. The
|
| 520 |
|
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|a potential vorticity values descended to levels below 400 hPa.
|
| 520 |
|
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|a Rockies, and rapid cyclogenesis occurred following the
|
| 520 |
|
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|a streak propagating to the northeastward from the southwestern
|
| 520 |
|
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|a suitable for studying the development of the cutoff cyclone
|
| 520 |
|
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|a surface cyclone, interaction with an upper-level cyclone, the
|
| 520 |
|
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|a the central United States in association with a deepening
|
| 520 |
|
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|a the indirect circulation in the exit region of the ULJ; Q-
|
| 520 |
|
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|a the interaction of these phenomena during the period 16-18
|
| 520 |
|
|
|a trough in the lee of the Rockies and an upper-level jet (ULJ)
|
| 520 |
|
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|a United States. The LLJ was coupled to the return branch of
|
| 520 |
|
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|a upper-tropospheric front. The cutoff cyclone became
|
| 520 |
|
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|a using existing theories concerning the development of a
|
| 520 |
|
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|a vector convergence indicated that the LLJ was driven by
|
| 520 |
|
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|a westerly current when the potential vorticity maximum became
|
| 530 |
|
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|a Also available online.
|
| 530 |
|
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|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-R576
|z Link to OAKTrust copy
|t 0
|
| 999 |
|
|
|a MARS
|
| 999 |
f |
f |
|s a491c9f6-2022-31fd-9287-3b29afc26122
|i 7bf93c39-adc0-3dae-a20c-7c235b7acaa5
|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 R576
|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 R576
|h Other scheme
|
| 998 |
f |
f |
|a 1995 Thesis R576
|t 0
|l Cushing: Theses & Dissertations Microforms (Does not check out)
|
| 998 |
f |
f |
|a 1995 Thesis R576
|t 0
|l Available Online
|