Deserts 265 15 Deserts Topics A. What are the principles that apply to the atmosphere as concerns the transfer of moisture? B. What are Hadley and Ferrel cells? How do they explain the occurrence of subtropical deserts? C. What are the explanations for deserts ascribed to rain shadows and cold-water coasts? What are two examples of how animals use principles of atmosphere dynamics? D. What is the practical de?nition of aridity? What is the de?nition of ‘evaporation index,’ and what E.I. value characterizes the Great American Desert? What are some of the erosional and depositional landforms that characterize deserts? What are four kinds of sand dunes, and how does each kind record the direction of wind that shaped it? E. What geologic history is recorded by features evident on the Lakeside, Nebraska quadrangle? A. The what and where of deserts—but ?rst, a few principles The locations of deserts are largely controlled by atmospheric circulation. Why? Because the agent that moves moisture from its principal source—the world ocean—onto the land, is wind. The capacity of air to obtain moisture from the ocean through evaporation, along with the effectiveness of air to deposit that moisture on land through condensation, involves the following four principles, which are illustrated in Figure 15.1. #1: Air obtains moisture from the ocean through evaporation of sea water. #2: Land absorbs solar energy more readily than does sea water, so air over a landmass is warmed to a greater degree than that over an adjacent ocean. #3: Warm air is less dense than cold air, so warm air tends to rise, and cold tends to sink. #4: Warm air has a greater moistureholding capacity than does cold air, so as warm air is cooled it tends to lose moisture (as rain or snow). Q 15.1 Where moisture-laden air moves from sea to land, which is almost everywhere the case, (a) it is heated by the warmer land, (b) made less dense, and (c) caused to rise. At higher elevations moisture within the air condenses, producing clouds and rain. Review: In one sentence, why the condensation? #4 Rising air is cooled (because of decreasing atmospheric pressure) Moisture condenses, forming clouds and rain #3a Warm air is less dense, so it rises #2 Warm land adds heat to air #3b Cold air is more dense, so it sinks #1 Air over an ocean acquires moisture through evaporation; moves inland, replacing rising land air Figure 15.1 This simple model illustrates principles #1 through #4. 266 Deserts B. Global Subtropical deserts From the principles discussed and illustrated on the previous page, it follows that rising air promotes rainfall, and descending air promotes dryness. That simple principle pretty much explains the geography of deserts. As everyone knows, heat from the sun is greater in equatorial regions than in polar regions. But why? Two reasons, both of which are illustrated in Figure 15.2: First, solar energy per unit area of Earth’s surface is greater at low latitudes. Second, the greater angle of incidence of solar energy at low latitudes results in less loss via re?ection of that energy. E qu a t or Cooler, more dense air sinks ey ce ll dl As we have already seen, the heating of air causes it to expand, thereby making it less dense, which causes it to rise. This phenomenon, known as convection, lifts hot-air balloons. Figure 15.2 At lower latitudes (a) solar energy is more concentrated (i.e., there is more heat energy per unit area), and (b) re?ection of that energy into space is less. Ha The most extensive deserts on Earth are associated with two circumglobal belts of descending air between 20° and 30° north and south latitudes. Notable examples of these subtropical deserts include the Sahara and Kalahari of Africa, the Rub-al-Khali of Saudi Arabia, the Sind of Iran in the Northern Hemisphere, and the Great Australian Desert in the Southern Hemisphere. But why deserts within these particular latitude belts? ift rd dr a tw es W Warmer, less dense air rises Eastward rotation Equator tw d ar ift dr Figure 15.3 A Hadley cell would be the simple consequence of solar heating, were it not for the fact that Earth is rotating. The bold arrows schematically show the tendency for westward drift of atmospheric and ocean currents owing to Earth’s eastward rotation. es W The Hadley cell—From the preceding paragraph, it follows that warmer, less dense air in equatorial regions tends to rise, and cooler, more dense air in polar regions tends to sink (Fig. 15.3). This simplistic model of global circulation is known as the Hadley cell, named for George Hadley (1685–1768), the British physicist who ?rst envisioned the mechanism. But the plot thickens. The Hadley cell as it is illustrated in Figure 15.3 would be the case were Earth not rotating. But Earth is rotating, which causes atmospheric and ocean currents to drift westward (see bold arrows in Figure 15.3). Q15.2. On page 277 of the Answer Page, sketch Hadley cells for the other three quadrants on the two-dimensional view of Earth. Deserts 267 Ferrel’s three-cell model for each hemisphere derives in large part from Earth’s 24-hour period of rotation. Other planets have different angular velocities. For example, Jupiter turns on its axis once every 11 hours. The Ferrel cell—An elaboration of Hadley’s model, which takes Earth’s rotation into account, was proposed by U.S. meteorologist William Ferrel in 1865 (Fig. 15.4). Ferrel’s model explains the world’s great subtropical deserts. Earth’s rotation can be viewed as breaking up an otherwise single Hadley cell into three cells: Hadley, Ferrel, and Polar. Wind directions with east west components (e.g., Northeast trades, Southeast trades, and Westerlies) occur between adjacent cells. Figure 15.4 The three-cell model of William Ferrel—which includes Hadley, Ferrel, and Polar cells in each hemisphere—best explains the paths of winds nearest the ground. Q15.3 How many cells do you suppose Jupiter has in each hemisphere relative to those of Earth—fewer, equal, or more? Hint: If cells are broken into smaller cells by rotation, what’s your intuitive guess as to the result of faster and faster rotation? (Disregard the relative sizes of Earth and Jupiter.) Dry cold air, more dense, sinks. cell lar Po North pole Wet Fe rr e lc el l 60° N latitude Dry W e s te r l i e s 30° N latitude High cell High Northeast trades Hadley Moist hot air, less dense, rises. Equatorial low Equator Wet y Hadle Southeast trades cell High High 30° S latitude Dry Westerlies Fe rre ell lc 60° S latitude Wet Pol ar c e ll South pole National Oceanic and Atmospheric Administration home page is at http://www.ncdc.noaa.gov 268 Deserts C. Regional causes of deserts Rain shadows—Where atmospheric circulation drives prevailing winds across a mountainous region, arid or semi-arid conditions commonly occur on the leeward side in what is called a ‘rain shadow’ (Fig. 15.5). Windward side (wet) Leeward side rain shadow (dry) Mountains Lowlands Figure 15.5 Where prevailing winds move across a mountain range, humid conditions occur on the windward side, and dry conditions occur on the leeward side. Q15.4 Given principles 1–4 on page 265, explain the occurrence of the two contrasting climates illustrated in Figure 15.5. Cold-water coasts—Coastal land is almost invariably warmer than adjacent ocean water; so, the warmer air over a coast usually rises, and cooler ocean air moves in to replace it (again, see Figure 15.1). The resulting onshore breeze accounts for the sur?ng industry and for coastal trees leaning landward. Where coastal waters ?ow from either Arctic or Antarctic regions, air above the water is exceedingly cold, to the extent that it cannot hold appreciable moisture. So, even though the air moves onto warmer land, gains heat, and therefore rises, precipitation seldom occurs. Deserts result (Fig. 15.6). Little moisture to form clouds (dry conditions) Cold, dry air rt Dese itions cond Warmer land Cold ocean Figure 15.6 A cold-water coast illustrating the reason for arid conditions. Deserts 269 Figure 15.7 shows two great deserts, the Great American Desert and the PeruChilean Desert, along with prevailing westerly wind in North America and the exceptionally cold Humbolt current offshore of Peru and Chile. Q15.5. On page 277 of the Answer Page construct topographic pro?les along lines A-B and C-D in Figure 15.7. For each, indicate with arrows the air circulation that accounts for the related desert. Label each of your pro?les so as to match it with one of the ?gures on facing page 268 (i.e., include in each of your pro?les either labels from Figure 15.5 or labels from Figure 15.6). B Great American Desert A Figure 15.7. Map of two Western Hemisphere deserts showing relevant westerly wind in North America and relevant Humbolt ocean current offshore of South America. Peru-Chilean Desert D C Animals know about air. Soaring birds apply one of the principles in Figure 15.1 on page 265. Q15.6. When a hawk or eagle wishes to gain altitude after a tiring day of hunting, that bird heads for a spot beneath a cumulus cloud. Why? Hint: What is the motion of air beneath a cumulus cloud? What accounts for the cloud development? Prairie dog architects mound dirt around their entrances/exits to provide a watch tower and to turn away surface water. But they build some mounds much higher than others. One theory is that the higher mounds assure ventilation within the village, thanks to the Bernoulli principle. Q15.7. How does the Bernoulli principle apply to the architecture of a prairie dog village? Hint: Ever hear of an airfoil—the shape of an airplane wing that gives it lift? Air str Airfoil Air stream eam Air in Wind Air out 270 Deserts D. Desert landscapes The Great American Desert The de?nition of aridity is not based on precipitation alone (e.g., 10 cm or less per year). Aridity also depends on evaporation. Practically speaking, a region is viewed as arid where potential evaporation exceeds annual precipitation, which includes some 30% of Earth’s land surface. A more scienti?c measure of dryness is the evaporation index (Fig. 15.17), which is inches of potential annual evaporation divided by inches of actual annual precipitation. The Great American Desert of our western states is characterized by values in excess of 2.5 on the E.I. scale. Desert landscapes occur within this region. Desert hazards In addition to the issue of water, arid regions pose special hazards: Sudden dust storms—As blinding as ‘whiteout’ snow storms. Figure 15.8 Desert landscapes of our conterminous 48 states occur within areas where the evaporation index is in excess of 2.5. Evaporation index 2.5 3.0 3.5 5.0 Flash ?oods—Arid regions present special ?ash-?ood hazards. An arid-lands hiker strolling along an arroyo (Fig. 15.9) can be unaware of a distant rainstorm before being confronted by a wall of water. Figure 15.9. Arroyos are ?at-?oored stream channels with steep walls. Occasional water evaporates and soaks into the dry earth—depositing sediments en route, creating a ?at channel ?oor. Surprisingly chilly nights—Arid regions typically exhibit surprising differences in daytime/nighttime temperatures. About ?ash ?oods…in Almería Province, Spain—the driest spot in all Europe—a concrete-?oored and concrete-walled arroyo passes through the center of coastal Almería town en route to the Mediterranean Sea (Fig. 15.10). Local geologists 15.8 Why are nights in arid lands quip that there is a “delta of car bodies” offshore of Almería. surprisingly cold? Hint: Think of a feature of the atmosphere that holds 15.9 So how do you suppose this delta of car bodies developed? Hint: To daytime heat during the night. what use do you imagine drivers put this concrete arroyo? (It’s a universal need in urban settings and on college campuses.) Maze-like corridors—One can easily become lost in the narrow passages of badlands (i.e., rugged arid landscapes). Cartagena Ebenezer Bryce, from whom Bryce Canyon National Park takes its name, once quipped that his canyon was “a hell of a place to lose a cow.” Granada Q Q S P A I N Almería M 0 0 ed ite r ea ran n Sea N 50 km Figure 15.10 Car bodies rest in their watery grave offshore of Almería, Spain. 50 mi Deserts 271 Desert erosion In those deserts where sediments are effectively carried away by occasional rainwater, imposing spires and spines of rock rise above ?at valley ?oors. An example is famous Monument Valley, Arizona (Fig. 15.11). Countless western movies have been ?lmed here. Q15.10 Draw a topographic pro?le along the segmented white line in Figure 15.11. Also, show, with a geologic cross-section beneath your topographic pro?le, three horizontal rock layers rising from the ?at valley ?oor. Label the lowest and highest layers (i.e., the cliff formers) sandstone and the one red sloping layer between them shale. Q15.11 Draw a circle around an abrupt spire standing like a ‘monu- ment,’ an example of the features that give this area its name. Q15.12 In Monument Valley erosion is along parallel fractures (called joints), which imparts a topographic fabric. Three or four ‘peninsular’ spines exhibit a mutual orientation. What is their approximate azimuth in a northerly direction? (See ‘azimuths’ on page 35.) Desert erosion Monument Valley, Arizona N.J. MD. Mystery Valley, Arizona-Utah 7 1/2’ quadrangle N 1 mi N. 36° 55’ 21’’, W. 110° 08’ 39’’ 1 km D A B C Figure 15.11 Removal of sediments from this desert area by occasional rainwater has produced ‘islands’ and ‘peninsulas’ of ?at-lying layers of sedimentary rocks. 272 Deserts Desert deposition Deposition by water—Deserts are characterized by a lack of vegetation because (a) there is insuf?cient water to sustain plants, and (b) there is insuf?cient water for chemical weathering of bedrock to produce nutrient-rich soil. Without plants to obstruct the ?ow of surface water, and without porous soil to absorb that water, runoff of rainwater is at a maximum—resulting in ?ash ?oods. However, ?ood waters in deserts quickly evaporate and/or soak into what little dry soil there is, so sediments are dumped along stream courses, burying hills and, in some cases, mountains as well (Fig. 15.12). The landscape in ?gure 15.12 is quite different from that in ?gure 15.11. The bedrock in ?gure 15.11 consists of layered sedimentary rocks, so the ?at valley ?oor might very well owe its occurrence to a horizontal layer of rock. But in ?gure 15.12 the bedrock appears Desert deposition California to consist of massive plutonic igneous rock, without a layer or layers that might explain the ?at valley ?oors. Q15.13. Draw a cross-section along line A–B in ?gure 15.12. Show both the surface topography and your guess as to the boundary between the partially-buried mountains and the sediments. Hint: View the sediments as a lake that has partially drowned a hilly landscape. N.J. MD. Frink NW, California, 7 1/2’ quadrangle 1/4 km N. 33° 25’ 03’’, W. 115° 37’ 39’’ A B Figure 15.12. Desert mountains become buried in their own debris. N 1/4 mi Deserts 273 Deposition by wind—The word desert brings to mind sand dunes, of which there are several types. The most common is the barchan dune (Fig. 15.13), in which the horns of this crescentshaped dune point downwind. Figure 15.14 is a Google Earth image of a part of the Salton Sea of California, (Not the most of de?nitive photo, but such is desert imagery.) Occasional rain reduces bedrock to sand, which is then fashioned by wind into dunes. A B Q15.14 According to ?gure 15.13, what is the prevailing wind direction indicated by dune A in ?gure 15.14? Q15.15 Do the dunes in Figure 15.14 re?ect recent movement (i.e., within historical time), or have they been stationary for, say, a thousand years? Give two lines of evidence for your answer. Hint: (A) One line of evidence is indicated by the distribution of vegetation in front of a dune compared with that behind it. (Give the letter label of such a dune and explain.) (B) The other line of evidence is indicated by the relationship between a particular dune and a cultural feature. Name that dune. Q15.16 Notice in Figure 15.14 that Figure 15.13 Barchan dune aerodynamics. A Map view with arrows indicating air ?ow. A constant wind direction produces a dune that is symmetrical in plan view. B Oblique view. some of the dunes are not perfectly symmetrical like that shown in ?gure 15.13 (e.g., dune A). (A) Describe this asymmetry, and (B) try to explain it. Hint: See caption to ?gure 15.13A. N 1/2 mi 1/2 km D MD. C A Sand dunes Salton Sea, California E B Kane Spring NE, California, 7 1/2’ quadrangle N. 33° 11’ 05’’, W. 115° 50’ 58’’ Figure 15.14 Sand dunes near Kane Spring, California, are typically of the barchan variety. But horns point in a variety of directions. Does this re?ect changing wind directions? 274 Deserts Types of sand dunes—Sand dunes come in a variety of shapes (Fig. 15.15). Three shapes—barchan, parabolic, and transverse—indicate wind direction. Barchan and parabolic dunes appear in map view to have contradictory shapes, but there is one universality among the three types of dune shapes that indicate wind direction: The windward side is the gentler slope, and the leeward side is the steeper slope. So their cross-sections are more de?nitive of wind direction than are their shapes in map view. A longitudinal dune is ambiguous; wind direction can be either of two directions parallel to the dune’s long axis. WIND Windward (up-wind side) Map view Leeward (down-wind side) Cross-sections Another product of wind erosion is a depression called a blowout. Unlike running water, both glacial ice and wind can scoop out soil and rock creating closed depressions, which, where ?lled by water, become natural lakes. Q15.17 On page 278 of the Answer Page draw a topographic pro?le from coordinates F-6.7 to H.5-10 on the Lakeside quadrangle. Q15.18 Which is the steeper side of this dune—the northwest side or the southeast side? Q15.19 Which kind of dune illusE. An ancient desert: Lakeside, Nebraska The Lakeside, Nebraska, quadrangle on facing page 275 covers part of an area of Pleistocene (aka The Ice Age) sand dunes that have long since been overgrown and stabilized by grass. But these fossil dunes still exhibit much of their original shapes. As a guide to the study of sand dunes on the Lakeside quadrangle, Figure 15.16 shows an idealized contour map of a dune. trated in Figure 15.15 do you believe you traversed with your topographic pro?le? Q15.20. From which direction did the wind that fashioned the dunes of the Lakeside region blow (NE, NW, SE, or SW)? Q15.21 What is there about the shape of the dune in your topographic pro?le that indicates that this is an ancient dune, rather than an active dune on the move? Barchan Parabolic 50 40 30 Figure 15.15. Four types of dunes. Three of the shapes—barchan, parabolic, and transverse—indicate wind direction by their steeper slopes being on their leeward sides. 20 Longitudinal 10 0 Transverse Figure 15.16. Idealized contour map of a sand dune 50+ feet high. The base of the dune is arbitrarily assigned the value of 0 feet. Deserts 275 276 Deserts Intentionally blank Deserts 277 (Student’s name) (Lab instructor’s name) (Day) (Hour) ANSWER PAGE 15.5 15.1 A C 15.2 15.6 Ha dl c ? ey l el 15.7 Equator ? ? 15.3 15.8 15.4 B D 278 Deserts 15.16 15.9 15.10 A B D C 15.17 (Lakeside, Nebraska, Quadrangle—page 275) F-6.7 Feet 4100 15.11 15.12 4000 15.13 3900 A B 15.18 15.19 15.14 15.20 15.15 (A) 15.21 (B) H.5-10 Hide preview glg101r4_Week_4_Deserts_Worksheet.doc Download Attachment This is an unformatted preview. Please download the attached document for the original format. Deserts Worksheet | 1 GLG/101 Version 4 Associate Level Material Deserts Worksheet Answer the lab questions for this week and summarize the lab experience using this form. Carefully read Ch. 15 of Geoscience Laboratory. Complete this week’s lab by filling in your responses to the questions from Geoscience Laboratory. Although you are only required to respond to the questions in this worksheet, you are encouraged to answer others from the text on your own. Questions and charts are from Geoscience Laboratory, 5th ed. (p. 265-275), by T. Freeman, 2009, New York, NY: John Wiley & Sons. Reprinted with permission. Lab Questions: 15.4 Given principles 1–4 on page 265, explain the occurrence of the two contrasting climates illustrated in Figure 15.5. The two contrasting climates are wet on the windward side and dry on the leeward side. From the principles I learned that in high elevations the evaporated moisture produces clouds and rain, which is why the windward side is wet. At the lower elevations the evaporated moisture as it rises it dissipates due to the humidity and does not produce clouds like the windward side. As the air s 15.8 Why are nights in arid lands surprisingly cold? Hint: Think of a feature of the atmosphere that holds daytime heat during the night. This happens because the air is dry and can’t retain the heat that is prevalent during the daytime. 15.16 Notice in Figure 15.14 that some of the dunes are not perfectly symmetrical like that shown in Figure 15.13. (A) Describe this asymmetry, and (B) try to explain it. Hint: Study the caption to Figure 15.13A. Deserts Worksheet | 2 GLG/101 Version 4 15.17 On page 278 of the Answer Page (below) draw a topographic profile from coordinates F-6.7 to H.5-10 on the Lakeside quadrangle. 15.18 Which is the steeper side of this dune—the northwest side or the southeast side? 15.19 Which kind of dune illustrated in Figure 15.15 do you believe you traversed with your topographic profile? Lab Summary: Address the following in a 200-300 word summary: ? ? Summarize the general principles and purpose of the lab. Explain how this lab helped you better understand the topics and concepts addressed this week. ? Describe what you found challenging about this lab. ? Describe what you found interesting about this lab. Write your summary here: Hide preview Additional Requirements Min Pages: 1 Level of Detail: Show all work Other Requirements: I attached both documents needed to do this assignment.
