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Journal articles on the topic 'Southwestern'

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Author: Grafiati
Published: 4 June 2021
Last updated: 21 February 2023

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1

Tu, Chuan-Chi, Yi-Leng Chen, Shu-Ya Chen, Ying-Hwa Kuo, and Pay-Liam Lin. "Impacts of Including Rain-Evaporative Cooling in the Initial Conditions on the Prediction of a Coastal Heavy Rainfall Event during TiMREX." Monthly Weather Review 145, no. 1 (January 1, 2017): 253–77. http://dx.doi.org/10.1175/mwr-d-16-0224.1.

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Abstract A cycling run, which began 36 h before the model forecast, was employed to assimilate special Terrain-influenced Monsoon Rainfall Experiment (TiMREX) soundings, Global Telecommunications System (GTS) data, and Constellation Observing System for Meteorology, Ionosphere and Climate (COSMIC) global positioning system (GPS) radio occultation (RO) refractivity profiles to improve the model initial conditions provided by the National Centers for Environmental Prediction (NCEP) Global Forecast System (GFS) to study a coastal, heavy rainfall event over southwestern Taiwan during 15–16 June 2008. The 36-h cycling run with data assimilation (DA_ALL_DATA run) has a positive impact on the depiction of subsynoptic flow in the model initial conditions at 1200 UTC 15 June, including the warm moist tongue and southwesterly monsoon flow over the open ocean. Furthermore, the cold pool caused by the evaporative cooling of antecedent rains and orographic blocking over southwestern Taiwan are better resolved in the nested high-resolution domain in the DA_ALL_DATA run as compared to the initial conditions provided by the NCEP GFS. As a result, the heavy rainfall along the southwestern coast and afternoon localized heavy rainfall over northern Taiwan are better predicted in the DA_ALL_DATA run. Model sensitivity tests are also performed to diagnose the effects of terrain and rain-evaporative cooling on the intensity and depth of the cold pool and degree of orographic blocking on the southwesterly flow over southwestern Taiwan. It is apparent that including rain-evaporative cooling from antecedent rains and orographic effects in the model initial conditions are important to account for the predicted rainfall distribution of this coastal rainfall event.
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2

Tu, Chuan-Chi, Yi-Leng Chen, Ching-Sen Chen, Pay-Liam Lin, and Po-Hsiung Lin. "A Comparison of Two Heavy Rainfall Events during the Terrain-Influenced Monsoon Rainfall Experiment (TiMREX) 2008." Monthly Weather Review 142, no. 7 (June 27, 2014): 2436–63. http://dx.doi.org/10.1175/mwr-d-13-00293.1.

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Abstract Two contrasting localized heavy rainfall events during Taiwan’s early summer rainy season with the daily rainfall maximum along the windward mountain range and coast were studied and compared using a combination of observations and numerical simulations. Both events occurred under favorable large-scale settings including the existence of a moisture tongue from the tropics. For the 31 May case, heavy rainfall occurred in the afternoon hours over the southwestern windward slopes after a shallow surface front passed central Taiwan. The orographic lifting of the prevailing warm, moist, west-southwesterly flow aloft, combined with a sea breeze–upslope flow at the surface provided the localized lifting needed for the development of heavy precipitation. On 16 June before sunrise, pronounced orographic blocking of the warm, moist, south-southwesterly flow occurred because of the presence of relatively cold air at low levels as a result of nocturnal and rain evaporative cooling. As a result, convective systems intensified as they moved toward the southwestern coast. During the daytime, the cold pool remained over southwestern Taiwan without the development of onshore/upslope flow. Furthermore, with a south-southwesterly flow aloft parallel to terrain contours, orographic lifting aloft was absent and preexisting rain cells offshore diminished after they moved inland. Over northern Taiwan on the lee side, a sea breeze/onshore flow developed in the afternoon hours, resulting in heavy thundershowers. These results demonstrate the importance of diurnal and local effects on determining the location and timing of the occurrences of localized heavy precipitation during the early summer rainy season over Taiwan.
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3

KOJI, TAKEHIKO. "Southwestern histochemistry." Newsletter of Japan Society for Comparative Endocrinology, no. 94 (1999): 19–23. http://dx.doi.org/10.5983/nl2001jsce.25.94_19.

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4

Dunn, Jeff. "Southwestern Collection." Southwestern Historical Quarterly 119, no. 4 (2016): 406–30. http://dx.doi.org/10.1353/swh.2016.0027.

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5

Ding, Xiaonan, Ling Fu, Ping Guan, and Daowei Zhang. "The Southwestern Boundary of Cenozoic Qaidam Basin: Constraints from Heavy Mineral Analysis." Minerals 12, no. 6 (June 16, 2022): 768. http://dx.doi.org/10.3390/min12060768.

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The formation of the Qaidam Basin plays an important role in unraveling the growth history of the Tibetan plateau. An extraordinary thick Cenozoic sedimentary succession of the Qaidam Basin is a great contributor to the study of the basin’s evolution history. To date, there has been disagreement on the southwestern boundary of the Paleogene Qaidam Basin. In this study, the method of heavy mineral analysis was adopted to reconstruct the southwestern boundary of the Qaidam Basin. The stable heavy minerals which represent the maturity of detrital sediments can roughly reflect the distance between the source and the deposit area. Therefore, the isogram of the stable heavy mineral index (ZTR = 20) was compiled to infer the location of the source area of the southwestern Qaidam Basin. The isogram shows that the boundary of the southwestern Qaidam Basin stretched southwesterly to the present-day Qiman Tagh Eastern Kunlun Mountains during the Paleogene. Additionally, the isolines present a remarkable northward migration since the late Eocene, which indicates the boundary of the Cenozoic Qaidam Basin that withdrew northward since the late Eocene. The specific location of the southern source area of the Qaidam Basin can be deduced at the Adatan fault, the middle of the present-day Eastern Kunlun Mountains. This result also supports the idea that the Qaidam Basin was an independent basin during the early Cenozoic era, and the Eastern Kunlun Mountains have already been exhumed during that time, serving as a prominent source of clastic sediments in the southwestern Qaidam Basin.
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6

K.J.G. "Southwestern Historical Association." Americas 45, no. 3 (January 1989): 418. http://dx.doi.org/10.1017/s0003161500075763.

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7

V.C.P. "Southwestern Studies Fellowships." Americas 52, no. 2 (October 1995): 229–30. http://dx.doi.org/10.1017/s0003161500023919.

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8

Hübscher, Ulrich. "Double replica southwestern." Nucleic Acids Research 15, no. 13 (1987): 5486. http://dx.doi.org/10.1093/nar/15.13.5486.

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9

Gilman, Patricia A. "Southwestern Archaeological Thought." American Anthropologist 97, no. 4 (October 28, 2009): 811–13. http://dx.doi.org/10.1525/aa.1995.97.4.02a00330.

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10

Pittayaporn, Pittayawat. "Layers of Chinese Loanwords in Protosouthwestern Tai as Evidence for the Dating of the Spread of Southwestern Tai." MANUSYA 17, no. 3 (2014): 47–68. http://dx.doi.org/10.1163/26659077-01703004.

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The current ethno-linguistic landscape of mainland Southeast Asia is a result of the spread of Tai speakers from southern China. This study examines Chinese loanwords in Proto-Southwestern Tai, the hypothetical ancestor of all modern Southwestern Tai varieties and proposes a dating of the spread of Southwestern Tai languages. By comparing the reconstructed Proto-Southwestern Tai forms with corresponding Chinese forms, four layers of Chinese loanwords existed in Proto- Southwestern Tai, namely Pre-Later Han, Later Han Chinese, Early Middle Chinese, and Late Middle Chinese layers. These layers indicate that Proto-Southwestern Tai was in contact with Chinese at least until the Tang era. In collaboration with non-linguistic evidence, this paper therefore proposes that Southwestern Tai languages began to spread southward sometime during the eighth and the tenth centuries CE.
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11

CUTHBERT, JENNIFER. "University of Texas Southwestern Medical Center at Dallas Southwestern Medical School." Academic Medicine 75, Supplement (September 2000): S363—S365. http://dx.doi.org/10.1097/00001888-200009001-00107.

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12

Trenhaile, Alan S. "Lacustrine shore platforms in southwestern Ontario, Canada." Zeitschrift für Geomorphologie 48, no. 4 (December 15, 2004): 441–59. http://dx.doi.org/10.1127/zfg/48/2004/441.

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13

Witmer, Robert, and Charlotte J. Frisbie. "Southwestern Indian Ritual Drama." Yearbook for Traditional Music 18 (1986): 173. http://dx.doi.org/10.2307/768528.

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14

Sweet, Jill, and Charlotte J. Frisbie. "Southwestern Indian Ritual Drama." Dance Research Journal 19, no. 2 (1987): 49. http://dx.doi.org/10.2307/1478177.

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15

Duncan, Elmer. "THE SOUTHWESTERN PHILOSOPHICAL SOCIETY." Southwest Philosophy Review 14, no. 1 (1998): 187–94. http://dx.doi.org/10.5840/swphilreview199814121.

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16

Llobera, Josep R. "Fieldwork in Southwestern Europe." Critique of Anthropology 6, no. 2 (July 1986): 25–33. http://dx.doi.org/10.1177/0308275x8600600203.

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17

Tanner, Clara Lee. "Southwestern Indian Gold Jewelry." KIVA 50, no. 4 (January 1985): 201–18. http://dx.doi.org/10.1080/00231940.1985.11758038.

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18

WAIT, JULIETTE. "Southwestern Internal Medicine Conference." American Journal of the Medical Sciences 310, no. 3 (September 1995): 118–25. http://dx.doi.org/10.1097/00000441-199509000-00007.

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19

McGuire, Randy, and Frank G. Anderson. "Southwestern Archaeology: A Bibliography." American Indian Quarterly 9, no. 2 (1985): 214. http://dx.doi.org/10.2307/1184592.

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20

Shackley, M. Steven, Paul E. Minnis, and Charles L. Redman. "Perspectives on Southwestern Prehistory." American Indian Quarterly 16, no. 1 (1992): 113. http://dx.doi.org/10.2307/1185629.

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21

Leavitt, Duane L. "Skarns of Southwestern Maine." Rocks & Minerals 62, no. 6 (November 1987): 429–32. http://dx.doi.org/10.1080/00357529.1987.11762700.

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22

Rubin, Craig D. "Southwestern Internal Medicine Conference." American Journal of the Medical Sciences 318, no. 3 (September 1999): 158. http://dx.doi.org/10.1097/00000441-199909000-00011.

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23

Weissler, Jonathan C. "Southwestern Internal Medicine Conference." American Journal of the Medical Sciences 319, no. 3 (March 2000): 166–76. http://dx.doi.org/10.1097/00000441-200003000-00006.

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24

Coyle, Yvonne M. "Southwestern Internal Medicine Conference." American Journal of the Medical Sciences 319, no. 4 (April 2000): 245–49. http://dx.doi.org/10.1097/00000441-200004000-00008.

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25

"Southwestern Collection." Southwestern Historical Quarterly 124, no. 3 (2021): 326–36. http://dx.doi.org/10.1353/swh.2021.0003.

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26

"Southwestern Collection." Southwestern Historical Quarterly 125, no. 1 (2021): 74–89. http://dx.doi.org/10.1353/swh.2021.0072.

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27

"Southwestern Collection." Southwestern Historical Quarterly 125, no. 4 (April 2022): 496–506. http://dx.doi.org/10.1353/swh.2022.0035.

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28

"Southwestern Collection." Southwestern Historical Quarterly 125, no. 3 (2022): 291–300. http://dx.doi.org/10.1353/swh.2022.0003.

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29

"Southwestern Collection." Southwestern Historical Quarterly 125, no. 2 (2021): 183–94. http://dx.doi.org/10.1353/swh.2021.0077.

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30

"Southwestern Collection." Southwestern Historical Quarterly 126, no. 2 (October 2022): 248–59. http://dx.doi.org/10.1353/swh.2022.0085.

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31

"Southwestern Collection." Southwestern Historical Quarterly 110, no. 4 (2007): 534–47. http://dx.doi.org/10.1353/swh.2007.0034.

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32

"Southwestern Collection." Southwestern Historical Quarterly 111, no. 1 (2007): 72–86. http://dx.doi.org/10.1353/swh.2007.0077.

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33

"Southwestern Collection." Southwestern Historical Quarterly 111, no. 2 (2007): 206–20. http://dx.doi.org/10.1353/swh.2007.0103.

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34

"Southwestern Collection." Southwestern Historical Quarterly 111, no. 3 (2008): 334–43. http://dx.doi.org/10.1353/swh.2008.0003.

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35

"Southwestern Collection." Southwestern Historical Quarterly 112, no. 1 (2008): 68–78. http://dx.doi.org/10.1353/swh.2008.0036.

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36

"Southwestern Collection." Southwestern Historical Quarterly 111, no. 4 (2008): 428–42. http://dx.doi.org/10.1353/swh.2008.0068.

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37

"Southwestern Collection." Southwestern Historical Quarterly 112, no. 2 (2008): 192–209. http://dx.doi.org/10.1353/swh.2008.0078.

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38

"Southwestern Collection." Southwestern Historical Quarterly 113, no. 1 (2009): 86–110. http://dx.doi.org/10.1353/swh.2009.0007.

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39

"Southwestern Collection." Southwestern Historical Quarterly 113, no. 2 (2009): 238–52. http://dx.doi.org/10.1353/swh.2009.0042.

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40

"Southwestern Collection." Southwestern Historical Quarterly 112, no. 4 (2009): 428–36. http://dx.doi.org/10.1353/swh.2009.0079.

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41

"Southwestern Collection." Southwestern Historical Quarterly 112, no. 3 (2009): 295–304. http://dx.doi.org/10.1353/swh.2009.0123.

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42

"Southwestern Collection." Southwestern Historical Quarterly 113, no. 3 (2010): 382–96. http://dx.doi.org/10.1353/swh.2010.0041.

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43

"Southwestern Collection." Southwestern Historical Quarterly 113, no. 4 (2010): 508–28. http://dx.doi.org/10.1353/swh.2010.0054.

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44

"Southwestern Collection." Southwestern Historical Quarterly 114, no. 3 (2011): 299–323. http://dx.doi.org/10.1353/swh.2011.0024.

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45

"Southwestern Collection." Southwestern Historical Quarterly 114, no. 4 (2011): 425–36. http://dx.doi.org/10.1353/swh.2011.0035.

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46

"Southwestern Collection." Southwestern Historical Quarterly 115, no. 1 (2011): 57–77. http://dx.doi.org/10.1353/swh.2011.0056.

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47

"Southwestern Collection." Southwestern Historical Quarterly 115, no. 2 (2011): 193–205. http://dx.doi.org/10.1353/swh.2011.0089.

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48

"Southwestern Collection." Southwestern Historical Quarterly 115, no. 3 (2012): 295–304. http://dx.doi.org/10.1353/swh.2012.0007.

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49

"Southwestern Collection." Southwestern Historical Quarterly 115, no. 4 (2012): 396–403. http://dx.doi.org/10.1353/swh.2012.0043.

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50

"Southwestern Collection." Southwestern Historical Quarterly 116, no. 1 (2012): 50–77. http://dx.doi.org/10.1353/swh.2012.0075.

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