FMFRP 0-54 the Persian Gulf Region, a Climatological Study
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Tectonics of the Musandam Peninsula and Northern Oman Mountains: from Ophiolite Obduction to Continental Collision
GeoArabia, 2014, v. 19, no. 2, p. 135-174 Gulf PetroLink, Bahrain Tectonics of the Musandam Peninsula and northern Oman Mountains: From ophiolite obduction to continental collision Michael P. Searle, Alan G. Cherry, Mohammed Y. Ali and David J.W. Cooper ABSTRACT The tectonics of the Musandam Peninsula in northern Oman shows a transition between the Late Cretaceous ophiolite emplacement related tectonics recorded along the Oman Mountains and Dibba Zone to the SE and the Late Cenozoic continent-continent collision tectonics along the Zagros Mountains in Iran to the northwest. Three stages in the continental collision process have been recognized. Stage one involves the emplacement of the Semail Ophiolite from NE to SW onto the Mid-Permian–Mesozoic passive continental margin of Arabia. The Semail Ophiolite shows a lower ocean ridge axis suite of gabbros, tonalites, trondhjemites and lavas (Geotimes V1 unit) dated by U-Pb zircon between 96.4–95.4 Ma overlain by a post-ridge suite including island-arc related volcanics including boninites formed between 95.4–94.7 Ma (Lasail, V2 unit). The ophiolite obduction process began at 96 Ma with subduction of Triassic–Jurassic oceanic crust to depths of > 40 km to form the amphibolite/granulite facies metamorphic sole along an ENE- dipping subduction zone. U-Pb ages of partial melts in the sole amphibolites (95.6– 94.5 Ma) overlap precisely in age with the ophiolite crustal sequence, implying that subduction was occurring at the same time as the ophiolite was forming. The ophiolite, together with the underlying Haybi and Hawasina thrust sheets, were thrust southwest on top of the Permian–Mesozoic shelf carbonate sequence during the Late Cenomanian–Campanian. -
Oman: Politics, Security, and U.S
Oman: Politics, Security, and U.S. Policy Updated May 19, 2021 Congressional Research Service https://crsreports.congress.gov RS21534 SUMMARY RS21534 Oman: Politics, Security, and U.S. Policy May 19, 2021 The Sultanate of Oman has been a strategic partner of the United States since 1980, when it became the first Persian Gulf state to sign a formal accord permitting the U.S. military to use its Kenneth Katzman facilities. Oman has hosted U.S. forces during every U.S. military operation in the region since Specialist in Middle then, and it is a partner in U.S. efforts to counter terrorist groups and other regional threats. In Eastern Affairs January 2020, Oman’s longtime leader, Sultan Qaboos bin Sa’id Al Said, passed away and was succeeded by Haythim bin Tariq Al Said, a cousin selected by Oman’s royal family immediately upon Qaboos’s death. Sultan Haythim espouses policies similar to those of Qaboos and has not altered U.S.-Oman ties or Oman’s regional policies. During Qaboos’s reign (1970-2020), Oman generally avoided joining other countries in the Gulf Cooperation Council (GCC: Saudi Arabia, Kuwait, United Arab Emirates , Bahrain, Qatar, and Oman) in regional military interventions, instead seeking to mediate their resolution. Oman joined but did not contribute forces to the U.S.-led coalition against the Islamic State organization, nor did it arm groups fighting Syrian President Bashar Al Asad’s regime. It opposed the June 2017 Saudi/UAE- led isolation of Qatar and had urged resolution of that rift before its resolution in January 2021. -
Weather Numbers Multiple Choices I
Weather Numbers Answer Bank A. 1 B. 2 C. 3 D. 4 E. 5 F. 25 G. 35 H. 36 I. 40 J. 46 K. 54 L. 58 M. 72 N. 74 O. 75 P. 80 Q. 100 R. 910 S. 1000 T. 1010 U. 1013 V. ½ W. ¾ 1. Minimum wind speed for a hurricane in mph N 74 mph 2. Flash-to-bang ratio. For every 10 second between lightning flash and thunder, the storm is this many miles away B 2 miles as flash to bang ratio is 5 seconds per mile 3. Minimum diameter of a hailstone in a severe storm (in inches) A 1 inch (formerly ¾ inches) 4. Standard sea level pressure in millibars U 1013.25 millibars 5. Minimum wind speed for a severe storm in mph L 58 mph 6. Minimum wind speed for a blizzard in mph G 35 mph 7. 22 degrees Celsius converted to Fahrenheit M 72 22 x 9/5 + 32 8. Increments between isobars in millibars D 4mb 9. Minimum water temperature in Fahrenheit for hurricane development P 80 F 10. Station model reports pressure as 100, what is the actual pressure in millibars T 1010 (remember to move decimal to left and then add either 10 or 9 100 become 10.0 910.0mb would be extreme low so logic would tell you it would be 1010.0mb) Multiple Choices I 1. A dry line front is also known as a: a. dew point front b. squall line front c. trough front d. Lemon front e. Kelvin front 2. -
Arabian Sea and the Gulf of Oman by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO
An Atlas of Oceanic Internal Solitary Waves (February 2004) Arabian Sea and the Gulf of Oman by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Arabian Sea and the Gulf of Oman Overview The Arabian Sea is located in the northwest Indian Ocean. It is bounded by India (to the east), Iran (to the north) and the Arabian Peninsula (in the west)(Figure 1). The Gulf of Oman is located in the northwest corner of the Arabian Sea. The continental shelf in the region is widest off the northwest coast of India, which also experiences wind-induced upwelling. [LME, 2004]. The circulation in the Arabian Sea is affected by the Northeast (March-April) and Southwest (September -October) Monsoon seasons [Tomczak et al. 2003]. Figure 1. Bathymetry of Arabian Sea [Smith and Sandwell, 1997]. 501 An Atlas of Oceanic Internal Solitary Waves (February 2004) Arabian Sea and the Gulf of Oman by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Observations There has been some scientific study of internal waves in the Arabian Sea and Gulf of Oman through the use of satellite imagery [Zheng et al., 1998; Small and Martin, 2002]. The imagery shows evidence of fine scale internal wave signatures along the continental shelf around the entire region. Table 1 shows the months of the year when internal wave observations have been made. Table 1 - Months when internal waves have been observed in the Arabian Sea and Gulf of Oman (Numbers indicate unique dates in that month when waves have been noted) Jan Feb Mar Apr May Jun Jul Aug Sept Oct Nov Dec 2 552 1251 Small and Martin [2002] reported on internal wave signatures observed in ERS SAR images of the Gulf of Oman. -
RSIS COMMENTARIES RSIS Commentaries Are Intended to Provide Timely And, Where Appropriate, Policy Relevant Background and Analysis of Contemporary Developments
RSIS COMMENTARIES RSIS Commentaries are intended to provide timely and, where appropriate, policy relevant background and analysis of contemporary developments. The views of the authors are their own and do not represent the official position of the S.Rajaratnam School of International Studies, NTU. These commentaries may be reproduced electronically or in print with prior permission from RSIS. Due recognition must be given to the author or authors and RSIS. Please email: [email protected] or call (+65) 6790 6982 to speak to the Editor RSIS Commentaries, Yang Razali Kassim. __________________________________________________________________________________________________ No. 81/2011 dated 18 May 2011 Indian Ocean Region: Critical Sea Lanes for Energy Security By Joshua Ho Synopsis The Indian Ocean region is home to three critical sea lanes used for global energy transportation. The disruption of these sea lanes, even temporarily, can lead to substantial increases in energy costs. What actions are required to keep these sea lanes safe? Commentary CHOKEPOINTS are narrow channels along widely used global sea routes. They are a critical part of global energy security due to the high volume of oil traded through their narrow straits. The Strait of Hormuz, leading out of the Persian Gulf, and the Strait of Malacca linking the Indian and the Pacific Oceans are two of the world’s most strategic chokepoints. They lie in the Indian Ocean region. Another important passage in the Indian Ocean region is the Bab el-Mandab, which connects the Arabian Sea and the Red Sea which leads to the Suez Canal. As the international energy market is dependent on reliable transport, the blockage of a chokepoint, even temporarily, can lead to substantial increases in total energy costs. -
Variations in Winter Surface High Pressure in the Northern Hemisphere and Climatological Impacts of Diminishing Arctic Sea Ice
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Earth and Atmospheric Sciences, Department Atmospheric Sciences of 5-2010 Variations in Winter Surface High Pressure in the Northern Hemisphere and Climatological Impacts of Diminishing Arctic Sea Ice Kristen D. Fox University of Nebraska at Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geoscidiss Part of the Other Earth Sciences Commons Fox, Kristen D., "Variations in Winter Surface High Pressure in the Northern Hemisphere and Climatological Impacts of Diminishing Arctic Sea Ice" (2010). Dissertations & Theses in Earth and Atmospheric Sciences. 8. https://digitalcommons.unl.edu/geoscidiss/8 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. VARIATIONS IN WINTER SURFACE HIGH PRESSURE IN THE NORTHERN HEMISPHERE AND CLIMATOLOGICAL IMPACTS OF DIMINISHING ARCTIC SEA ICE by Kristen D. Fox A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Geosciences Under the Supervision of Professor Mark Anderson Lincoln, Nebraska May, 2010 VARIATIONS IN WINTER SURFACE HIGH PRESSURE IN THE NORTHERN HEMISPHERE AND CLIMATOLOGICAL IMPACTS OF DIMINISHING ARCTIC SEA ICE Kristen D. Fox, M.S. University of Nebraska, 2010 Advisor: Mark Anderson This study explores the role Arctic sea ice plays in determining mean sea level pressure and 1000 hPa temperatures during Northern Hemisphere winters while focusing on an extended period of October to March. -
Arabian Peninsula from Wikipedia, the Free Encyclopedia Jump to Navigationjump to Search "Arabia" and "Arabian" Redirect Here
Arabian Peninsula From Wikipedia, the free encyclopedia Jump to navigationJump to search "Arabia" and "Arabian" redirect here. For other uses, see Arabia (disambiguation) and Arabian (disambiguation). Arabian Peninsula Area 3.2 million km2 (1.25 million mi²) Population 77,983,936 Demonym Arabian Countries Saudi Arabia Yemen Oman United Arab Emirates Kuwait Qatar Bahrain -shibhu l-jazīrati l ِش ْبهُ ا ْل َج ِزي َرةِ ا ْلعَ َربِيَّة :The Arabian Peninsula, or simply Arabia[1] (/əˈreɪbiə/; Arabic jazīratu l-ʿarab, 'Island of the Arabs'),[2] is َج ِزي َرةُ ا ْلعَ َرب ʿarabiyyah, 'Arabian peninsula' or a peninsula of Western Asia situated northeast of Africa on the Arabian plate. From a geographical perspective, it is considered a subcontinent of Asia.[3] It is the largest peninsula in the world, at 3,237,500 km2 (1,250,000 sq mi).[4][5][6][7][8] The peninsula consists of the countries Yemen, Oman, Qatar, Bahrain, Kuwait, Saudi Arabia and the United Arab Emirates.[9] The peninsula formed as a result of the rifting of the Red Sea between 56 and 23 million years ago, and is bordered by the Red Sea to the west and southwest, the Persian Gulf to the northeast, the Levant to the north and the Indian Ocean to the southeast. The peninsula plays a critical geopolitical role in the Arab world due to its vast reserves of oil and natural gas. The most populous cities on the Arabian Peninsula are Riyadh, Dubai, Jeddah, Abu Dhabi, Doha, Kuwait City, Sanaʽa, and Mecca. Before the modern era, it was divided into four distinct regions: Red Sea Coast (Tihamah), Central Plateau (Al-Yamama), Indian Ocean Coast (Hadhramaut) and Persian Gulf Coast (Al-Bahrain). -
A Comparative Analysis of Strategic Competition in the Middle East And
ense ef Ma f D n o a l g a e m Roudgar, J Def Manag 2017, 7:2 n r e u n o t J Journal of Defense Management DOI: 10.4172/2167-0374.1000164 ISSN: 2167-0374 ReviewResearch Article Article Open Access A Comparative Analysis of Strategic Competition in the Middle East and Asia-Pacific Iraj Roudgar* Department of Policy Studies, Universiti Teknologi Malaysia (UTM), Malaysia Abstract This study aimed to identify specific policies issues that contribute to the strategic competition in the Middle East and Asia-Pacific regions. It comprised the grand strategies of Iran, China, and North Korea -as pivotal regional actors- reactions in response to the USA military presence in the Persian Gulf, South China Sea, and Korean Peninsula. The conflicting security between the American global interests and regional powers’ interests has brought a sustainable competition in the world. The strategic competition has resulted in conflicting security and conflicts of policy objectives at the regional and global levels. The results also indicated that geopolitical dominance and an ability to launch nuclear weapons are the principal reasons for the strategic competition. Keywords: Alliances; Foreign policy; Grand strategy; Distribution of geographic choke point and main artery for the transport of oil from power; Strategic interests the Middle East. The USA imports are relativity little of the oil from the Strait of Hormuz, but two Americans alliances in Asia-Pacific such Introduction South Korea and Japan depended on the imports of crude oil. Thus, The conflicting security due to different kinds of regional and the stability of the Persian Gulf will remain an important focus of strategic interests and policy objectives at the regional and global levels Western strategy for many years to come. -
Part 2 Severe Weather
34 INTRODUCTION to SEVERE WEATHER (from http://www.srh.noaa.gov/jetstream//) 34 35 Chapter 1. Tropical Cyclone (from http://www.srh.noaa.gov/srh/jetstream/tropics/tropics_intro.htm) 1. Introduction A tropical cyclone is a warm-core, low pressure system without any "front" attached, that develops over the tropical or subtropical waters, and has an organized circulation. Depending upon location, tropical cyclones have different names around the world. In the: • Atlantic/Eastern Pacific Oceans - hurricanes • Western Pacific - typhoons • Indian Ocean - cyclones Regardless of what they are called, there are several favorable environmental conditions that must be in place before a tropical cyclone can form. They are: • Warm ocean waters (at least 80°F / 27°C) throughou t a depth of about 150 ft. (46 m). • An atmosphere which cools fast enough with height such that it is potentially unstable to moist convection. • Relatively moist air near the mid-level of the troposphere (16,000 ft. / 4,900 m). • Generally a minimum distance of at least 300 miles (480 km) from the equator. • A pre-existing near-surface disturbance. • Low values (less than about 23 mph / 37 kph) of vertical wind shear between the surface and the upper troposphere. Vertical wind shear is the change in wind speed with height. 35 36 Tropical Cyclone Formation Basin Given that sea surface temperatures need to be at least 80°F (27°C) for tropical cyclones form, it is natural that they form near the equator. However, with only the rarest of occasions, these storms do not form within 5° latitude of the equator. -
Understanding the Dominant Sources and Tracks of Moisture for Summer
Journal of Geophysical Research: Atmospheres RESEARCH ARTICLE Understanding the Dominant Sources and Tracks of Moisture 10.1029/2017JD027652 for Summer Rainfall in the Southwest United States Key Points: Srijita Jana1,2 , Balaji Rajagopalan1,2 , Michael A. Alexander3 , and Andrea J. Ray3 • The leading source of moisture varies depending on the part of the region 1Department of Civil, Environmental and Architectural Engineering, University of Colorado Boulder, Boulder, CO, USA, • Land is an important source of 2 3 moisture during the summer season Cooperative Institute of Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA, NOAA • Large-scale circulation features are Earth System Research Laboratory, Boulder, CO, USA consistent with major pathways of moisture Abstract We investigated the moisture sources and tracks that enable summer rainfall over the four-state Supporting Information: southwestern U.S. region of Arizona, New Mexico, Colorado, and Utah by employing a high-resolution • Supporting Information S1 Lagrangian particle tracking model. Six locations were selected—Cedar City (Utah), Grand Junction • Table S1 (Colorado), Eastonville (Colorado), Laveen (Arizona), Redrock (New Mexico), and Melrose (New Mexico) • Table S2 —together, they represent six spatial regions of summer precipitation for the Southwest. Moisture tracks – Correspondence to: were generated for all the rainy days at these stations for the historical period 1979 2013. Tracks were S. Jana and B. Rajagopalan, generated for a 3-day period ending with the day of rainfall, which were then used to identify the [email protected]; source of moisture, pathway or trajectory, and the modulation along the track. The four major sources of [email protected] moisture—Gulf of California, Gulf of Mexico (GoM), land, and the Pacific Ocean—were identified as responsible for summer rainfall over southwestern United States. -
Extratropical Storms of the Gulf of Mexico and Their Ffece Ts Along the Northern Coast of a Barrier Island: West Ship Island, Mississippi
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1999 Extratropical Storms of the Gulf of Mexico and Their ffecE ts Along the Northern Coast of a Barrier Island: West Ship Island, Mississippi. Phillip Lynn Chaney Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Chaney, Phillip Lynn, "Extratropical Storms of the Gulf of Mexico and Their Effects Along the Northern Coast of a Barrier Island: West Ship Island, Mississippi." (1999). LSU Historical Dissertations and Theses. 6884. https://digitalcommons.lsu.edu/gradschool_disstheses/6884 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type o f computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. -
A Reconstructed Siberian High Index Since A.D. 1599 from Eurasian And
GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L05705, doi:10.1029/2004GL022271, 2005 A reconstructed Siberian High index since A.D. 1599 from Eurasian and North American tree rings Rosanne D’Arrigo,1 Gordon Jacoby,1 Rob Wilson,2 and Fotis Panagiotopoulos3 Received 20 December 2004; revised 17 January 2005; accepted 2 February 2005; published 2 March 2005. [1] The long-term variability of the Siberian High, the Precipitation correlations are coherent over large regions of dominant Northern Hemisphere anticyclone during winter, Eurasia, and highest near the Urals. is largely unknown. To investigate how this feature varied [4] Despite its spatial extent, the SH has attracted less prior to the instrumental record, we present a reconstruction attention than other circulation features such as the North of a Dec–Feb Siberian High (SH) index based on Eurasian Atlantic Oscillation or NAO [S1991; Cohen et al., 2001; and North American tree rings. Spanning 1599–1980, it P2005]. The SH’s interactions with features of global provides information on SH variability over the past four climate, including the NAO, Arctic Oscillation (AO) [Wu centuries. A decline in the instrumental SH index since the and Wang, 2002], East Asian winter monsoon (EAWM), late 1970s, related to Eurasian warming, is the most striking Aleutian Low, and El Nin˜o-Southern Oscillation (ENSO) feature over the past four hundred years. It is associated are still not well understood [e.g., P2005]. Of the major with a highly significant (p < 0.0001) step change in 1989. teleconnection patterns of the Northern Hemisphere, the SH Significant 3–4 yr spectral peaks in the reconstruction fall is best correlated with the AO (r = À0.48, Dec–Feb 1958– within the range of variability of the East Asian winter 98 [Gong and Ho, 2002]).