PH- portland headlandmap on left- is a section of a coastline off .pdf

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PH- portland headland map on left- is a section of a coastline off UK(channel) Map on right- contours of relative potential vorticity (units of f, planetary vorticity) that has averaged over no. of tidal cycles the map shows the main direction of tidal flow is shown (ebb/ flood tides) explain how the average relative vorticity distribution is produced, and make a diagram that shows the mean residual flow that may be produced/generated by the tidal flow past PH QUESTION 2 there is a diagram below below that shows a period of time of the movement of tides and water across a W->EAST slope in N Hemisphere The flood tide causes a movement of water to -> shallow end of slope (labelled h) & ebb tide the deeper end of slope (labelled H) DESCRIBE & explain using conservation of potential vorticity how the relative vorticity causes imbalance/change in the period during 2 tidal stages and which may cause an iniation of a residual flow along the slope with shallow water to -> right.

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1. Carcfully and neuely celor alluvial fan A yellins. inchading the places at the tep (voploge end) of the fan where it eusends up into iwi canyons. Do the uame for alluvial fans B and C . 2. Coloc the inselbergs broen in the viritity of loxation D . 1. Colow the 00 (sea Ifved) topopraphic condoves the on beah sider of the valley. 1. Make as urange line along the downhall edge of the monteain thowe (Fig. 15.7) an both sides of the valley. What is the elevation ef the kouced point en the map? f Totice the inlermittent stream that diains from the upstream end of the allavial fan systemt A (that you have already colored ellowy to the playa at E. How wodld the grain sise of the sediments aleog this stream change as you walk downslope from th. ighest part of the fan, up in the canyons, to the playa (E)? Why? arefully examine Fig. A15.4.1 for evidence of normal faults on either or both sides of Death Valley. Refer to Fig. 15.10 for eas. Draw a dark dahbod line with a repular pencil or a Black coloeed pencil wherever yoe think a normal fault might reach th ound surface on either the east of west side of the valley. Imost a decade of meaweements indicate that relative to the sakle intener of the North Aamerican Plate (N.LD06). GPS site 462 mones toward ariinuth 309. 7 at a rate of 3.90 mavlyr, and site P996 moves tonsard 315.5 5 at 5.39 mmlyr (ycllow rows in Fig 15. 10). Both GPS sites are part of the Plast Boundary Observatony developed as purt of the Earthscope Preject. Selative to P462. GPS sile P596 moves tow and 327. 1 at 1.95 menyt (ocange arrow in Fig. 15.10). Block faulting typital of the Basin and fange tendi to itviodve tarelching neughly perpendicalar to mormal fadtus as shewn in the arange arrow oniginating at GPS sine PS96 in Fig. 15.10 that shows the molion of the wees side of Dearh Valley relative to the easa side, is the current widening of Death Valley more hively relised to Becin and-Range block fuelting oe to developmemt of a pell-apart hasin? Explain your rexenning. The strie-slip faulis to the noth and sowh of Death Valley kave been astive for atonat 12 Myr (Fig. 15.10) If psog moved in the aame difection at the same rate relative ss P46z for 12 Myz , how far would PSh move? Aboet how far is it fram the bedrock on the east side of the valley to the top ef the allevial slope on the weat side of the valley measures parallel to the orange arrow and the oeanfe strike-slip faults? kin FLET 8 DISCUSS Notice thar poople chose to build a ranch on alfuvial fan B even though this enline region is dry What do you think was the single most important reason why thene people chose alluvial fan B for their ranch instead of of the other fans? A. Analyre the topographic map in Fig. A15.4.1 and complele the follensing lakks. Refer to Fig. 15 for guidacke. .

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There are two types of currents in the ocean: 1) surface currents move the water above the pycnocline a) ≈ 10% of the ocean b) horizontal motion c) wind powered = solar powered 2) thermohaline = deep currents move the water below the pycnoline (zone of rapid change of water density) a) ≈ 90% of the ocean b) horizontal and vertical motion c) density driven density depends temperature and salinity these are also solar powered 3) these two sets of current are interconnected Chapter 7 – Ocean Circulation Surface currents are moved by friction between the surface winds and the water surface = wind driven. max speed is 3% of wind speed Since winds are solar powered, surface currents are solar powered. The overall pattern of surface currents is controlled by the Coriolis effect, gravity, and the shape of the ocean basin. Like Fig 7.7, p. 205 Ekman Transport – the net (or average) motion of wind driven water, is 90° to the direction of the wind. In a perfect world, this movement is: 90° to the right in the Northern Hemisphere, 90° to the left in the Southern Hemisphere, WHY?...........the Coriolis Effect Fig. 9-, p. 236 In the northern hemisphere, the Westerlies tends to move water southeast, while the Trade winds move water northwest! wind direction wind-driven water movement (Ekman Transport) The Westerlies (30° - 60°) and the Trade Winds (0° – 30°) are the strongest winds,* and are the main winds causing ocean currents! Largest change in temperature causes the strongest wind! Remember, according to Ekman Transport, wind - driven water moves 90° to the wind direction. In the northern hemisphere, the Westerlies tends to move water southeast, while the Trade winds move water northwest! The movement of wind-driven water can be described with a vector = an arrow pointing in the direction of travel and scaled to the speed. This vector can be broken up into a component moving toward the edge of the ocean and a component moving toward the center of the ocean. wind direction water movement vectors of water movement The water moving east or west (toward the edge of the basin) bounces off of the land. In the northern hemisphere, the water current turns right! Current bounces off land Current bounces off land Subtropical Convergence = a short (≈ 6.5 feet tall) hill of water formed when part of the wind blow water moves to the center of the ocean basin. Can water stand in a hill? No! Gravity works to move the water back downhill. BUT the wind is still working to push water uphill again So – The winds build the hill taller, and The taller the hill the more gravity pulls the water back downhill The hill continues to grow until wind driven Coriolis deflected motion in = gravity driven motion out. Then – only the circular movement around the edge of the hill is left. THIS IS THE SURFACE CURRENT! Garrison, 2009, Essentials of Oceanography Under the hill of wa ...

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FucueE 10.13 Pattern of tcour and deposition within canyons of Big Thompson and North Fork. Big Thampson rivers. Floedway is about 200 in wide with grastats of 24 percent ishroba et al, 1979 . 19. The heavist peecipitation from this fload secured enough time. The river determines how much time is between 1930 and 2040 hours MDT at Glen Comfort and "enough"; it may be a few years, a few decades, or a 1930 and 2200 hours at Clen Haven. There was lute oppor. few centuries. But over time, rivers will occupy and turity to wam anyone. Uie this intormation with the other modify their floodplains. information in this exercise to prepare two paragraphs, one On a shorter tiene period, floods will cover parts apguing for and the other againet parchave of a waterfront of the tiver valley. How much gets covered is deterlot for a houne in one of the miny river valleys er canyons mined by how big the floods are. similar to Big Thompson along the Front Range of the Fockies. Uae a aeparate sheet is paper for your anwwer. QUESTIONS (10, PART D) Refer to Figure 2.10 in Chapter 2 . Blooningted, Indiana. 1. Sketh a toposraphic profile of the valley of Griffy Creck. Meandering Rivers and Identification of Flood Township 16 in the East. Mark the floodplain oe the profile Plains on Topographic Maps The first step in avoiding flood hazards is to avoid building in rivers. Some geoscientists suggest that the area known as the food plain should instead jast be 2. Is the Drive-in Theater (Southwest of the dami) in a floodcalled part of the river. The implication of this is important. Food plains are natural parts of river syotems that do not happen to be covered by water alf of the time. When flood plains are covered by watec, however, the damage to unprepared (and in some 3. E Payne Cemetery (east-central part of the mapy in a cases even prepared) people and communities can be disastrous. In this part of the exescise we are going to use several diffenent topographic maps in the colored plates section of the book, and identify differtent flood plains on the maps. First, refer to Figure 10.14, which is a sketch of typical topographic features seen along a flood plain. Note on this figure that natural rivens meander (bend) a lot. The floodplain is the topograptically low area adjacent to the river. Although when we look at a river it may appeat to have a permanent charnel, meandering rivers will change their channels and erode and redeposit over their entire floodplain, givem.

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OTEL: RIXOS PREMIUM BELEK OTEL POZSYON: PAZARLAMA EKB COVID-19'dan nce seyahat ve turizm, kresel GSYH'nn yzde 10'unu ve dnya apnda 320 milyondan fazla istihdam oluturan dnya ekonomisinin en nemli sektrlerinden biri haline gelmiti. Yeni bir birbirine ballk anda leinin ilk rnei olan kresel salgn, ou mikro, kk ve orta lekli iletmelerde ve turizmin yzde 54'n temsil eden yksek oranda kadn istihdam eden 100 milyon ii riske att. Birlemi Milletler Dnya Turizm rgt'ne (UNWTO) gre i gc. Turizme baml lkeler, krizin olumsuz etkilerini muhtemelen dier ekonomilere gre ok daha uzun sre hissedecekler. Turizm ve seyahat sektrlerinin kilit noktas olan temas youn hizmetler, pandemiden orantsz bir ekilde etkileniyor ve insanlar yeniden toplu halde seyahat etme konusunda kendilerini gvende hissedene kadar mcadele etmeye devam edecek. Dnya apnda turizm gelirlerinin 2023 ylna kadar 2019 seviyelerine kmas beklenmiyor. Bu yln ilk yarsnda, turist girileri kresel olarak yzde 65'ten fazla dt ve Nisan ayndan bu yana neredeyse durdu - kresel mali kriz srasnda yzde 8 ve yzde 17 idi. Pandemi sonras dnyada turizm zerine devam eden IMF aratrmasna gre, 2003'teki SARS salgn srasnda yzde. AMA: otelin pandeminin sonuna kadar ayakta kalmasna ve en popler otellerden biri olmak iin korona sonras dneme hazrlanmasna yardmc olacak en iyi stratejilere karar vermek ?.

OTEL RIXOS PREMIUM BELEK OTEL POZSYON PAZARLAMA EKB COVID-19d.pdf

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other information provided is the answer for T T=-0.62 i still ne.pdf

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Please complete the fill in the box exercise by identify the federal regulation or initiative used to combat fraud and abuse described in the following table. Example: Amendment Right to Bear Arms 2nd amendment Example of fraud and abuse Federal regulation or initiative Known as the Physician Self-Referral Law (4 points) Qui tam is the whistleblower provision (4 points) Also known as HEAT (4 points) Physicians cannot receive money or other benefits for referring patients to a healthcare facility (4 points) The office in the federal government that works to combat fraud, waste, and abuse (4 points) Amendment Right to Bear Arms 2nd amendment.

Please complete the fill in the box exercise by identify the federal.pdf

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