| LDR | | 01925nmm uu200373 4500 |
| 001 | | 000000334276 |
| 005 | | 20240805180001 |
| 008 | | 181129s2016 |||||||||||||||||c||eng d |
| 020 | |
▼a 9780438135093 |
| 035 | |
▼a (MiAaPQ)AAI10903684 |
| 040 | |
▼a MiAaPQ
▼c MiAaPQ
▼d 248032 |
| 082 | 0 |
▼a 551 |
| 100 | 1 |
▼a Jensen, Anders A. |
| 245 | 10 |
▼a Modeling Ice Particle Aspect Ratio Evolution During Riming. |
| 260 | |
▼a [S.l.] :
▼b The Pennsylvania State University.,
▼c 2016 |
| 260 | 1 |
▼a Ann Arbor :
▼b ProQuest Dissertations & Theses,
▼c 2016 |
| 300 | |
▼a 140 p. |
| 500 | |
▼a Source: Dissertation Abstracts International, Volume: 79-12(E), Section: B. |
| 502 | 1 |
▼a Thesis (Ph.D.)--The Pennsylvania State University, 2016. |
| 520 | |
▼a The first part of this dissertation describes and tests a single-particle ice growth model that evolves both ice crystal mass and shape as a result of vapor growth and riming. Columnar collision efficiencies in the model are calculated using a n |
| 520 | |
▼a Part two details a novel bulk microphysics model that simultaneously evolves mass, shape, and density due to both riming and vapor growth. A direct result is that conversion rates between, for example, snow and graupel, are not needed. The metho |
| 520 | |
▼a In part three the microphysics parameterization is tested in a WRF squall line case. The results show that the modeling approach to ice microphysics successfully captures features of the squall line including the transition zone and enhanced str |
| 590 | |
▼a School code: 0176. |
| 650 | 4 |
▼a Meteorology. |
| 690 | |
▼a 0557 |
| 710 | 20 |
▼a The Pennsylvania State University.
▼b Meteorology. |
| 773 | 0 |
▼t Dissertation Abstracts International
▼g 79-12B(E). |
| 773 | |
▼t Dissertation Abstract International |
| 790 | |
▼a 0176 |
| 791 | |
▼a Ph.D. |
| 792 | |
▼a 2016 |
| 793 | |
▼a English |
| 856 | 40 |
▼u http://www.riss.kr/pdu/ddodLink.do?id=T15000672
▼n KERIS |
| 980 | |
▼a 201812
▼f 2019 |
| 990 | |
▼a 관리자 |