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1

Kimball, E. "Desert Storm Environmental Effects." Journal of the IEST 35, no. 4 (1992): 30–33. http://dx.doi.org/10.17764/jiet.2.35.4.x4r6l3r8k9q68751.

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Recent forward deployment of an air defense system launch station resulted in the need to collect comprehensive new information on Saudi Arabian environmental extremes. This article includes a discussion on equipment reliability when it is exposed to abnormally high temperatures, severe dust storms, and salt fog which would be experienced during Desert Storm operations.
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2

West, Lola, Susan O. Mercer, and Edith Altheimer. "Operation Desert Storm:." Social Work in Health Care 19, no. 2 (1993): 81–98. http://dx.doi.org/10.1300/j010v19n02_04.

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3

Toma, J. S. "Desert Storm communications." IEEE Communications Magazine 30, no. 1 (1992): 19–21. http://dx.doi.org/10.1109/35.166643.

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4

Unkle, David W. "Images from Desert Shield and Desert Storm." Journal of Neuroscience Nursing 23, no. 6 (1991): 343–44. http://dx.doi.org/10.1097/01376517-199112000-00001.

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5

Simpson, Benny J., Billy W. Hipp, and Edward L. McWilliams. "‘White Storm’ and ‘Dark Storm’ Desert Willow." HortScience 24, no. 1 (1989): 178–79. http://dx.doi.org/10.21273/hortsci.24.1.178.

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Abstract Desert willow [Chilopsis linearis (Cav.) Sweet.] (7, 12) is a facultative phreatophyte (a plant whose roots will extract water from underground streams, a water table, or perched sources, or the strata immediately above these sources, but which can also function well in the absence of these water supplies). It is a tall shrub to a small tree (2, 3) and is native to the American southwest, from Baja California, southern California, southern Nevada, Arizona, and New Mexico to southwestern Texas and northern Mexico (8, 9).
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6

Perry, William J. "Desert Storm and Deterrence." Foreign Affairs 70, no. 4 (1991): 66. http://dx.doi.org/10.2307/20044914.

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7

Killick-Kendrick, R., and W. Peters. "Leishmaniasis and ‘Desert Storm’." Transactions of the Royal Society of Tropical Medicine and Hygiene 86, no. 6 (1992): 698. http://dx.doi.org/10.1016/0035-9203(92)90199-m.

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8

Manicom, David. "Desert Rose, Butterfly Storm." Review: Literature and Arts of the Americas 41, no. 1 (2008): 106–15. http://dx.doi.org/10.1080/08905760801979962.

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9

Myers, D. "Doctors and Desert Storm." BMJ 304, no. 6826 (1992): 576–77. http://dx.doi.org/10.1136/bmj.304.6826.576-b.

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10

Sarno, Albert P. "More on Desert Storm." JAMA: The Journal of the American Medical Association 266, no. 23 (1991): 3282. http://dx.doi.org/10.1001/jama.1991.03470230040014.

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11

Neish, Steven R. "More on Desert Storm." JAMA: The Journal of the American Medical Association 266, no. 23 (1991): 3282. http://dx.doi.org/10.1001/jama.1991.03470230040015.

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12

Middleton, Nick. "Dust storm hazards." E3S Web of Conferences 99 (2019): 04001. http://dx.doi.org/10.1051/e3sconf/20199904001.

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Dust storms originate in many of the world's drylands and frequently present hazards to human society, both within the drylands themselves but also outside drylands due to long-range transport of aeolian sediments. Desert dust hazards can occur where dust is entrained, during the transport phase, and on deposition. This paper draws on studies in physical geography, medical geology and geomorphology to discuss case studies of accelerated soil erosion, the health effects of air pollution caused by desert aerosols, injuries related to transport accidents caused by poor visibility during desert du
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13

Bao, Tana, Guilin Xi, Yanling Hao, et al. "The Transport Path and Vertical Structure of Dust Storms in East Asia and the Impacts on Cities in Northern China." Remote Sensing 15, no. 12 (2023): 3183. http://dx.doi.org/10.3390/rs15123183.

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Dust storm disasters have emerged as a significant environmental challenge in East Asia. However, relying on a single monitoring method to track dust storms presents limitations and can be variable. Therefore, it is necessary to use a combination of ground and remote sensing monitoring methods to explore the source and impact range of dust storms in order to fully characterize them. To achieve this, we examined the sources and impact ranges of dust storms in East Asia from 1980 to 2020 using both ground station data and remote sensing data. In addition, we focused on three specific dust storm
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14

Stewart, Richard W. "Operations Desert Shield and Desert Storm (Part I)." International Journal of Military History and Historiography 36, no. 2 (2016): 166–83. http://dx.doi.org/10.1163/24683302-03602004.

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This two-part historiographical article examines many of the key historical books written in English on military operations in the Persian Gulf from 1990 to 1991. Although increasingly viewed, even by historians, as little more than a historical footnote to the tumultuous events in the region after the 9/11 terrorist attacks and the subsequent invasion of Iraq in 2003, the events of the Persian Gulf War, often referred to by their U.S. operational names Operations Desert Shield and Desert Storm, have given us a rich and important literature on its military aspects of the war. The Gulf War was
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15

Stewart, Richard W. "Operations Desert Shield and Desert Storm (Part ii)." International Journal of Military History and Historiography 37, no. 1 (2017): 58–84. http://dx.doi.org/10.1163/24683302-03701005.

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This is the second of two parts of a review article on some of the key historical books written in English on military operations in the Persian Gulf from 1990 to 1991. Where the first part focused on the important operations and technological developments surrounding the air war, this second part discusses those works on the operations of ground (army and marines) and naval forces, professional studies, memoirs, some books on non-u.s. military operations, and finally some general or popular works on the war. Although increasingly viewed, even by historians, as little more than a historical fo
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16

Carver, Lord. "El Alamein to desert storm: Fifty years from desert to desert." RUSI Journal 137, no. 3 (1992): 52–56. http://dx.doi.org/10.1080/03071849208445606.

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17

Crase, Darrell. "Desert Storm: America at War." Illness, Crisis & Loss 1, no. 3 (1991): 27–33. http://dx.doi.org/10.2190/il1.3.e.

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18

Guenther, B. D., R. Buser, and W. Morrow. "Electro-optics in Desert Storm." Optics and Photonics News 2, no. 11 (1991): 8. http://dx.doi.org/10.1364/opn.2.11.000008.

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19

Salerno, D. P., and T. F. Washer. "Desert Storm: air assault communications." IEEE Communications Magazine 30, no. 1 (1992): 36–41. http://dx.doi.org/10.1109/35.166647.

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20

Fontenot, Gregory, Alberto Bin, Richard Hill, and Archer Jones. "Desert Storm: A Forgotten War." Journal of Military History 63, no. 4 (1999): 1051. http://dx.doi.org/10.2307/120635.

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21

Lipshitz, Raanan. "The Road to Desert Storm." Organization Studies 16, no. 2 (1995): 243–64. http://dx.doi.org/10.1177/017084069501600203.

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Analysis of escalation of commitment is used to highlight the differences between two paradigms in the study of decision making. The rational paradigm proposes that escalation is a dysfunctional response to failure (Staw and Ross 1987). A single-option paradigm, developed in this paper, proposes that it is a necessary response to uncertainty which may, but not necessarily, result in failure. Analysis of the decision-making process of President Bush prior to Operation Desert Storm highlights the differences between the two paradigms and demonstrates how they provide different interpretations an
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22

Hill, GeorgeJ. "Medical Planning - Desert Shield/Storm." Military Medicine 157, no. 10 (1992): A9. http://dx.doi.org/10.1093/milmed/157.10.a9.

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23

Nelson, Harold V. "Debt and Desert Shield/Storm." Military Medicine 158, no. 8 (1993): A6—A7. http://dx.doi.org/10.1093/milmed/158.8.a6a.

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24

Gunby, P. "Desert Storm--moves into history." JAMA: The Journal of the American Medical Association 265, no. 10 (1991): 1222. http://dx.doi.org/10.1001/jama.265.10.1222.

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25

Gunby, P. "Desert Storm data compilation continues." JAMA: The Journal of the American Medical Association 265, no. 16 (1991): 2045. http://dx.doi.org/10.1001/jama.265.16.2045.

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26

Nicolson, G. L. "Doxycycline treatment and Desert Storm." JAMA: The Journal of the American Medical Association 273, no. 8 (1995): 618–19. http://dx.doi.org/10.1001/jama.273.8.618.

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27

Keeler, Jill R. "More on Desert Storm-Reply." JAMA: The Journal of the American Medical Association 266, no. 23 (1991): 3283. http://dx.doi.org/10.1001/jama.1991.03470230040016.

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28

Davey, Basiro. "Desert Storm Syndrome and Immunization." Archives of Internal Medicine 156, no. 2 (1996): 217. http://dx.doi.org/10.1001/archinte.1996.00440020127023.

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29

Rosenberg-Nicolson, Nancy L. "Doxycycline Treatment and Desert Storm." JAMA: The Journal of the American Medical Association 273, no. 8 (1995): 618. http://dx.doi.org/10.1001/jama.1995.03520320026026.

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30

Gunby, Phil. "Desert Storm—Moves Into History." JAMA: The Journal of the American Medical Association 265, no. 10 (1991): 1222. http://dx.doi.org/10.1001/jama.1991.03460100012004.

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31

Gunby, Phil. "Desert Storm Data Compilation Continues." JAMA: The Journal of the American Medical Association 265, no. 16 (1991): 2045. http://dx.doi.org/10.1001/jama.1991.03460160019004.

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32

Reiber, H. "Desert Storm syndrome and immunization." Archives of Internal Medicine 156, no. 2 (1996): 217. http://dx.doi.org/10.1001/archinte.156.2.217.

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33

Aguilar, Germán, Albert Cabré, Victor Fredes, and Bruno Villela. "Erosion after an extreme storm event in an arid fluvial system of the southern Atacama Desert: an assessment of the magnitude, return time, and conditioning factors of erosion and debris flow generation." Natural Hazards and Earth System Sciences 20, no. 5 (2020): 1247–65. http://dx.doi.org/10.5194/nhess-20-1247-2020.

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Abstract. The contribution of an individual extreme storm event to long-term erosion rates has been estimated for the first time in the Atacama Desert. A mean erosion of 1.3 mm has been calculated for the March 2015 event that impacted the southernmost part of the Atacama Desert. The estimated erosion is consistent with millennial erosion rates and the previously reported return times of high-sediment-discharge events in the study area. This is significant because erosion rates, related to events of high sediment discharge in arid fluvial systems, are difficult to measure with sediment loading
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34

St John, Graham, and Botond Vitos. "Wurst Storm Rising." Journal of Festive Studies 3, no. 1 (2022): 177–99. http://dx.doi.org/10.33823/jfs.2021.3.1.57.

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Our subject is the legacy of Dada implicit to the Burning Man phenomenon. Animate in the provocative output of fin-de-siècle French Symbolist writer and puppeteer Alfred Jarry, and filtered through the antics of the San Francisco Cacophony Society, Dada is foundational to the cultural aesthetic of Burning Man, by which we mean the event in Nevada’s Black Rock Desert playa (Black Rock City) and a global network of “burn” events. We address the significance of the Cacophony Society expedition that inaugurated the desert phase of Burning Man in 1990, “Zone Trip # 4: Bad Day at Black Rock.” Integr
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35

Lytle, Mark, and Dilip Hiro. "Desert Shield to Desert Storm: The Second Gulf War." Journal of American History 80, no. 3 (1993): 1171. http://dx.doi.org/10.2307/2080567.

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36

Ellis, James. "EM Residents Used in Desert Storm and Desert Shield." Emergency Medicine News 26, no. 2 (2004): 4. http://dx.doi.org/10.1097/00132981-200402000-00004.

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37

SMITH, BARBARA JEAN. "The Nurse Executive in Operation Desert Shield/Desert Storm." Nursing Management (Springhouse) 24, no. 1 (1993): 68???70. http://dx.doi.org/10.1097/00006247-199301000-00013.

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38

DONOVAN, FRANCIS R. "Sealift's Role in Operations Desert Shield and Desert Storm." Naval Engineers Journal 103, no. 4 (1991): 61–63. http://dx.doi.org/10.1111/j.1559-3584.1991.tb00981.x.

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39

Sun, Jing, Hong Bo Liu, Li Qun Zhang, and Yong Feng Xu. "Experimental Study of the Application of Sodium Silicate in the Windbreak and Sand Fixation Engineering." Advanced Materials Research 1092-1093 (March 2015): 1243–46. http://dx.doi.org/10.4028/www.scientific.net/amr.1092-1093.1243.

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With the accelerated development of land desertification, sudden wind sand disaster, strong dust storm occurrence frequency more and more high.In the desert area where the alkali content in soil is low and there is existence of quicksand, the sand brick was prepared by using sodium silicate as chemical sand fixation adhesive materials and sodium fluosilicate as hardening agent, in order to improve the surface properties of desert land, control the spread of deserts and improve the environment of desert. In this paper, the suitable dosage of sodium fluosilicate and sodium silicate were studied,
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40

Aili, Aishajiang, Abdul Waheed, Xinfeng Zhao, and Hailiang Xu. "Establishing an Early Warning System for Dust Storms in Peri-Desert Regions." Environments 11, no. 4 (2024): 61. http://dx.doi.org/10.3390/environments11040061.

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The Taklimakan Desert in northwest China stands as a significant contributor to dust storms, with its fringe oases already designated as ecologically fragile due to the severe impacts of these storms. This study focuses on Moyu County, situated on the southwest edge of the Taklimakan Desert, examining the origin and transport pathways of dust storms from 2004 to 2021. The classification involves utilizing a 36 h backward trajectory model and the k-means clustering technique, resulting in three clusters displaying distinct transport pathways and entry directions. Air pollutant concentrations at
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41

Ghalib, Wadie Ahmed Mokbel, Almoliki Mohammed Mansoor, and Sajan Chimmikuttanda Ponnappa. "Environmental Factors that Influence the Geography of Yemen Leading to Dust and Sand Storms - A Case Study." Journal of Environmental Geography 14, no. 1-2 (2021): 24–37. http://dx.doi.org/10.2478/jengeo-2021-0003.

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Abstract In Yemen, the dust storm is a common phenomenon severely affecting the economy and health. Yemen is located in a semi-desert desert area, where dust and sand storms occur all year round, however they are the most common at summer (from June until the end of September). Coastal areas (Hajjah, Hoddeidah, Taiz, Lahg, Aden, Abyan, Shabwah and Hadramout) and desert areas (Marib and Al Jowf) are affected by dust and sandstorms almost all year round. The western and central governorates of Yemen are mountainous regions, but influenced by dust too. Dust storms in Yemen have an impact on human
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42

Kugler, Jacek, Lewis W. Snider, and William Longwell. "From Desert Shield To Desert Storm: Success, Strife, Or Quagmire?" Conflict Management and Peace Science 13, no. 2 (1994): 113–48. http://dx.doi.org/10.1177/073889429401300202.

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43

Cardinal, Peter A. "Health Service Support in Operations Desert Shield and Desert Storm." Military Medicine 157, no. 4 (1992): 175–79. http://dx.doi.org/10.1093/milmed/157.4.175.

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44

Hyams, Kenneth C., August L. Bourgeois, Joel Escamilla, James Burans, and James N. Woody. "The Navy Forward Laboratory during Operations Desert Shield/Desert Storm." Military Medicine 158, no. 11 (1993): 729–32. http://dx.doi.org/10.1093/milmed/158.11.729.

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45

Case, Frederic T., Christopher W. Hines, and Steven N. Satchwell. "Analysis of air operations during DESERT SHIELD and DESERT STORM." Naval Research Logistics 42, no. 4 (1995): 715–36. http://dx.doi.org/10.1002/1520-6750(199506)42:4<715::aid-nav3220420412>3.0.co;2-c.

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46

Amit, Rivka, Yehouda Enzel, Tamir Grodek, Onn Crouvi, Naomi Porat, and Avner Ayalon. "The role of rare rainstorms in the formation of calcic soil horizons on alluvial surfaces in extreme deserts." Quaternary Research 74, no. 2 (2010): 177–87. http://dx.doi.org/10.1016/j.yqres.2010.06.001.

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AbstractSoils in similar geomorphic settings in hyperarid deserts (&lt; 50 mm yr−1) should have similar characteristics because a negative moisture balance controls their development. However, Reg soils in the hyperarid southern Negev and Namib deserts are distinctly different. Soils developed on stable alluvial surfaces with only direct input of rainfall and dust depend heavily on rainfall characteristics. Annual rainfall amount can be similar (15–30 mm), but storm duration can drastically alter Reg soil properties in deserts. The cooler fall/winter and dry hot summers of the southern Negev D
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47

Dutch, Steven I. "A Geologist Goes to Desert Storm." Journal of Geological Education 41, no. 1 (1993): 43–51. http://dx.doi.org/10.5408/0022-1368-41.1.43.

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48

Quandt, William B., and Muhammad Faour. "The Arab World after Desert Storm." Foreign Affairs 73, no. 3 (1994): 171. http://dx.doi.org/10.2307/20046715.

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49

Weitz, Richard. "Jointness and desert storm: a retrospective." Defense & Security Analysis 20, no. 2 (2004): 133–52. http://dx.doi.org/10.1080/1475179042000219107.

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50

Locke, Kenneth. "EM Residents Used in Desert Storm." Emergency Medicine News 26, no. 3 (2004): 4. http://dx.doi.org/10.1097/00132981-200403000-00004.

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