The Intertropical Convergence Zone (ITCZ)

Total Page:16

File Type:pdf, Size:1020Kb

The Intertropical Convergence Zone (ITCZ) 9/19/2018 Dr. Hoch RGPL 103 Global Cities: Planning and Development Dr. Hoch Email: [email protected] 1 9/19/2018 2 9/19/2018 Earth’s Orbit Around Sun Aphelion Perihelion July 6 (12:00) Jan 3 (00:00) 152.5 Million Km 147.5 Mil. Km EARTH SUN Dates for 2010 Earth Rotation Earth’s axis N Pole Ecliptic Plane (Plane of earth revolution around sun) 23 1/2° 3 9/19/2018 Northern Hemisphere Seasons • Summer • North pole tilted toward Sun • Days are longer than the nights • Get more energy - higher temperatures •Fall • Neither pole tilted toward the Sun • Days about equal with nights • Less energy than in the summer • Cooler temperatures Northern Hemisphere Seasons cont. •Winter • North pole tilted away from the Sun • Days shorter than the nights • Get less energy-Cold temperatures • Spring • Neither pole tilted toward the Sun • Days about equal to nights • More energy than winter- Warmer temperatures 4 9/19/2018 Global regions • Tropics (23 ½°N ‐ 23 ½°S) • Low latitudes (30°N ‐ 30°S) • Mid latitudes (30°N ‐ 60°N and 30°S ‐ 60°S ) • High latitudes (60°N ‐ 90°N and 60°S ‐ 90°S ) 5 9/19/2018 Key positional relationships •Tropic of Cancer - 23 1/2° N •Highest latitude in the Northern Hemisphere that the suns vertical rays ever reach •Tropic of Capricorn- 23 1/2° S •Highest latitude in the Southern Hemisphere that the suns vertical rays ever reach •Arctic circle- 66 1/2° N •24 hrs of daylight-summer solstice •24 hrs of darkness at winter solstice •Antarctic circle- 66 1/2° S •24 hrs of daylight-winter solstice •24 hrs of darkness at summer solstice Circle of illumination 6 9/19/2018 Equinoxes and Solstices (2010) Day Date Sub‐solar Point Summer solstice June 21 23 1/2° N Autumnal equinox Sept 23 0° Winter solstice Dec 21 23 1/2° S Vernal equinox March 20 0° Equinox 7 9/19/2018 Solstices Solar Heating 1 3 = 33.3% Earth 1 1 = 100% SUN Higher latitudes get LESS ENERGY per unit of area 8 9/19/2018 Most of the Sun’s Energy is Received in the Equatorial Region of the Earth Global‐scale circulation system • The equatorial and tropical regions receive far more solar energy than the midlatitudes and polar regions • This heat energy is redistributed from warmer to colder areas by means of atmospheric air circulation (60%) and ocean currents (40%) 9 9/19/2018 Hypothetical non‐rotating earth circulation Idealized global circulation 10 9/19/2018 The global circulation model Consists of three ‘cells’ 1) Tropical cell 2) Midlatitude cell 3) Polar cell Midlatitude and subtropical jet streams 11 9/19/2018 Cross‐sectional view of jet streams BLUE arrows and lines represent areas or fronts of HIGH pressure and rotate clockwise RED arrows and lines represent areas or fronts of LOW pressure and rotate counter-clockwise Cyclic changes in upper air flow 12 9/19/2018 ITCZ World Map The Intertropical Convergence Zone (ITCZ) 13 9/19/2018 The Intertropical Convergence Zone (ITCZ) The Intertropical Convergence Zone (ITCZ), known by sailors as the doldrums or the calms, is the area encircling Earth near the Equator, where the northeast and southeast trade winds converge The location of the ITCZ gradually varies with the seasons, roughly corresponding with the location of the thermal equator As the heat capacity of the oceans is greater than air over land, migration is more prominent over land Over the oceans, where the convergence zone is better defined, the seasonal cycle is more subtle, as the convection is constrained by the distribution of ocean temperatures Worldwide Rainforest Depletion • Reported in 2012, more than 200,000 acres of rainforest are burned every day • That is more than 150 acres lost every minute of every day, or 78 million acres lost every year • More than 20 percent of the Amazon rainforest is already gone • More is severely threatened as he destruction continues 14 9/19/2018 Rainforests also help to stabilize Earth's climate They absorb carbon dioxide The reduce the effects of worldwide anthropogenic climate change They also home to about half of the species of plants and wildlife on the planet Tropic Of South East Cancer Asia Rain Forest Amazon Basin Rain Forest Congo Basin Tropic Rain Of Forest Capricorn https://news.mongabay.com/2014/12/tropical‐deforestation‐could‐disrupt‐rainfall‐globally/ 15 9/19/2018 Where is the world’s population? • Roughly 88 percent of the world’s population lives in the Northern Hemisphere, with about half north of 27 degrees north Rankin • Taking the northern and southern hemispheres together, on average the world’s Bill population lives 24 degrees from the equator CIA Factbook (2001) 16 9/19/2018 http://www.radicalcartography.net/ http://www.radicalcartography.net/ 17 9/19/2018 18 9/19/2018 19 9/19/2018 Global Population • Currently estimated to be 6,870,100,000 • The highest growth rate observed was during the 1950s, 60s and 70s, peaking in 1963 at 2.2% • US Census Bureau Projections show a steady decline in population growth rate • UN projections show a rise in growth rate US Census Bureau Total Global Population United Nations Developing vs. Developed http://gecon.yale.edu/ http://gecon.yale.edu/large-pixeled-contour-globe 20 9/19/2018 The World’s most Populated City Regions Rank Metropolitan area Country Population 1 Tokyo Japan 32,450,000 2 Seoul South Korea 20,550,000 3 Mexico City Mexico 20,450,000 4 New York City United States 19,750,000 5 Mumbai India 19,200,000 6 Jakarta Indonesia 18,900,000 7 São Paulo Brazil 18,850,000 8 Delhi India 18,600,000 9 Osaka‐Kobe‐Kyoto Japan 17,375,000 10 Shanghai People's Republic of China 16,650,000 Trends in population growth in Developing World • The world’s human population has increased nearly fourfold in the past 100 years • Each day 200,000 more people are added to the world food demand • It is projected to increase from 6.7 billion (2006) to 9.2 billion by 2050 – It took only 12 years for the last billion to be added, a net increase of nearly 230,000 new people each day, who will need housing, food and other natural resources • The largest population increase is projected to occur in Asia, particularly in China, India and Southeast Asia, accounting for about 60% and more of the world’s population by 2050 • The rate of population growth, however, is still relatively high in Central America, and highest in Central and part of Western Africa. – In relative numbers, Africa will experience the most rapid growth, over 70% faster than in Asia – In sub‐Saharan Africa, the population is projected to increase from about 770 million to nearly 1.7 billion by 2050 UN population Division, 2007 21 9/19/2018 What is the cause of such population growth in Developing World? • Intensified globalization • Resulting in rapid urban‐industrial capitalism • Clustering of producers and consumers results in urban agglomeration economies • This process leads to greater productivity and technological innovation • Thus, resulting in a snowball effect that stimulates urban industrial expansion • While there are many positives, the negatives spill over creating societal challenges and environmental consequences The Earth at Night Man‐made light shining at night is used as a metric to measure the amount of urban development 22 9/19/2018 23 9/19/2018 Central Place Theory • Provides a conceptual mechanism for understanding the role of the city as a service center. 24 9/19/2018 25 9/19/2018 26 9/19/2018 27 9/19/2018 28 9/19/2018 29 9/19/2018 30 9/19/2018 USA Deforestation 1620 ‐ 1925 31 9/19/2018 Boston, 1903 USGS 32 9/19/2018 Philadelphia 1898, USGS 1885 33 9/19/2018 Von Thunen’s Concentric Zone Theory of urban development Tysons Corner, Fairfax County, VA 34.
Recommended publications
  • Science Journals — AAAS
    SCIENCE ADVANCES | RESEARCH ARTICLE CLIMATOLOGY 2017 © The Authors, some rights reserved; Human-induced changes in the distribution of rainfall exclusive licensee American Association 1,2 2 for the Advancement Aaron E. Putnam * and Wallace S. Broecker of Science. Distributed under a Creative ’ A likely consequence of global warming will be the redistribution of Earth s rain belts, affecting water availability Commons Attribution ’ for many of Earth s inhabitants. We consider three ways in which planetary warming might influence the global NonCommercial distribution of precipitation. The first possibility is that rainfall in the tropics will increase and that the subtropics License 4.0 (CC BY-NC). and mid-latitudes will become more arid. A second possibility is that Earth’s thermal equator, around which the planet’s rain belts and dry zones are organized, will migrate northward. This northward shift will be a consequence of the Northern Hemisphere, with its large continental area, warming faster than the Southern Hemisphere, with its large oceanic area. A third possibility is that both of these scenarios will play out simultaneously. We review paleoclimate evidence suggesting that (i) the middle latitudes were wetter during the last glacial maximum, (ii) a northward shift of the thermal equator attended the abrupt Bølling-Allerød climatic transition ~14.6 thousand years ago, and (iii) a southward shift occurred during the more recent Little Ice Age. We also inspect trends in Downloaded from seasonal surface heating between the hemispheres over the past several decades. From these clues, we predict that there will be a seasonally dependent response in rainfall patterns to global warming.
    [Show full text]
  • An Observational Study of the Tropical Tropospheric Circulation
    An Observational Study of the Tropical Tropospheric Circulation Ioana M. Dima A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy University of Washington 2005 Program Authorized to Offer Degree: Department of Atmospheric Sciences University of Washington Graduate School This is to certify that I have examined this copy of a doctoral dissertation by Ioana M. Dima and have found that it is complete and satisfactory in all respects, and that any and all revisions by the final examining committee have been made. Chair of the Supervisory Committee: ______________________________________________________________________ John M. Wallace Reading Committee: ______________________________________________________________________ John M. Wallace ______________________________________________________________________ Dennis L. Hartmann ______________________________________________________________________ Edward S. Sarachik Date: ______________________ In presenting this dissertation in partial fulfillment of the requirements for the doctoral degree at the University of Washington, I agree that the Library shall make its copies freely available for inspection. I further agree that extensive copying of the dissertation is allowable only for scholarly purposes, consistent with “fair use” as prescribed in the U.S. Copyright Law. Requests for copying or reproduction of this dissertation may be referred to Proquest Information and Learning, 300 North Zeeb Road, Ann Arbor, MI 48106-1346, to whom the
    [Show full text]
  • Bjerknes, 1966: a Possible Response of the Atmospheric Hadley
    A possible response of the atmospheric Hadley circulation to equatorial anomalies of ocean temperature By J. BJERKNES, University of California, Los Angeles (Manuscript received January 18, 1966) ABSTRACT Weakness and temporary elimination of the equatorial easterly winds over the eastern and central Pacific in late 1957 and early 1958 brought about a brief cessation of equatorial upwelling which in turn caused the occurrence of above-normal surface water temperatures in the tropical Pacific from the American coast westward to the dateline. This sudden introduction of a large anomalous heat source for the atmosphere intensified its thermodynamic circulation, especially in the wintertime (northern) hemisphere. Record intensity of the westerlies resulted in the eastern North Pacific. The anomalous depth of the Low in the Gulf of Alaska had the downwind effect of weakening the Iceland Low and setting the stage for a cold winter in northern Europe. Introduction tion run faster than normal in the affected longitude sector and transport absolute angular The concept of the Hadley circulation as used momentum to the subtropical jet stream at a in this article refers to the rising motion at the faster rate than normal. The continued pole- thermal equator and simultaneous sinking mo- ward flux of absolute angular momentum and tion in the belt of subtropical highs mutually the downward flux of the same in the belt of connected by the equatorward component of surface westerlies can then also be assumed to the tradewinds in the lower troposphere and by maintain stronger than normal westerlies in the compensating flow away from the equator in middle latitudes of t,he longitude sector under the upper troposphere.
    [Show full text]
  • Stream Metabolism Heats Up
    news & views unique in its spatial collocation with a Karin Sigloch 4. Pierce, K. L. & Morgan, L. A. Geol. Soc. Am. Mem. 179, 1–54 (1992). massive pile of subducted lithosphere. Department of Earth Sciences, University of Oxford, 5. Smith, R. B. et al. J. Volcanol. Geoth. Res. 188, 26–56 (2009). Ying Zhou’s3 observations are thus Oxford, UK. 6. Sigloch, K., McQuarrie, N. & Nolet, G. Nat. Geosci. 1, 458–462 intriguing because they suggest the e-mail: [email protected] (2008). 7. Burdick, S. et al. Seismol. Res. Lett. 79, 384–392 (2008). existence of a semi-deep upwelling within 8. Sigloch, K. Geochem. Geophys. Geosyst. 12, Q02W08 (2011). a deep subduction setting. Her proposed Published online: 21 May 2018 9. Schmandt, B. & Lin, F. C. Geophys. Res. Lett. 41, 6342–6349 explanation, of passive, wet mantle (2014). https://doi.org/10.1038/s41561-018-0150-4 10. Cao, A. & Levander, A. J. Geophys. Res. 115, B07301 (2010). upwelling in reaction to sudden slab 11. Schmandt, B., Dueker, K., Humphreys, E. & Hansen, S. foundering, opens a window to explain References Earth Planet. Sci. Lett. 331, 224–236 (2012). surficial plume indicators and will hopefully 1. Morgan, W. J. Bull. Am. Assoc. Pet. Geol. 56, 203–213 (1972). 12. Gao, S. S. & Liu, K. H. J. Geophys. Res. 119, 6452–6468 (2015). motivate the broader geoscience disciplines 2. Christiansen, R. L., Foulger, G. R. & Evans, J. R. Geol. Soc. Am. 13. Nelson, P. L. & Grand, S. P. Nat. Geosci. 11, 280–284 (2018). Bull. 114, 1245–1256 (2002).
    [Show full text]
  • Pressure Belts
    Introduction to Constitution & Preamble | 1 GEOGRAPHY MASTER SERIES UNIT 1 Climatology The ‘Atmosphere’ Around Us What is Climatology? ● It is due to the atmosphere that living beings can perform photosynthesis and respiration Climatology is the study of the atmospheric conditions and related climate & weather phenomena. which is essential part of survival of all life on the Earth. The Earth has a radius of 6400 km, and possesses a ● As part of the hydrologic cycle, water spends narrow skin called atmosphere which is the air that a lot of time in the atmosphere, mostly as envelopes the earth which stretches upwards upto a water vapour. The atmosphere is an important maximum thickness of about 500 km. Ninety-nine per reservoir for water. cent of the gases that constitute the atmosphere, are ● Ozone in the upper atmosphere absorbs high- located below a height of 32 km. energy ultraviolet (UV) radiations coming Earth’s atmosphere protects us from incoming space from the Sun. This protects living beings debris like comets, asteroids that burn up before on the Earth’s surface from the Sun’s most reaching the planet’s surface, and blocks harmful harmful rays. short wavelength radiations from the Sun. The lower ● Along with the oceans, the atmosphere keeps boundary of the atmosphere is considered to lie on the Earth’s temperatures within an acceptable Earth’s surface, the upper boundary is the gradational range. Without an atmosphere, Earth’s transition into space. temperatures would be frigid at night and It blocks the outgoing long wave radiations to keep the scorching hot during the day.
    [Show full text]
  • Link to Full Thesis
    Changing Rains Down in Africa: Verifying Shifts in the Position of the Intertropical Convergence Zone Using a New Seasonal Rainfall Model A Thesis Presented by Molly Michael Wieringa to the Department of Earth and Planetary Sciences in partial fulfillment of the requirements for a degree with honors of Bachelor of Arts April 2019 Harvard College Table of Contents Table of Contents…………………………………………………………………………i Abstract ............................................................................................................................. iii List of Figures .................................................................................................................... v List of Tables .................................................................................................................... vii List of Equations .............................................................................................................. vii Acknowledgments ............................................................................................................. ix Introduction ....................................................................................................................... 1 1. Rainfall in Equatorial Africa ............................................................................... 1 2. Seasonality and the Intertropical Convergence Zone ........................................ 4 3. Literature Review .................................................................................................. 7 4. Motivation
    [Show full text]
  • An Analysis of the Effect of Topography on the Martian Hadley Cells
    An Analysis of the Effect of Topography on the Martian Hadley Cells The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Zalucha, Angela M, R. Alan Plumb, and R. John Wilson. “An Analysis of the Effect of Topography on the Martian Hadley Cells.” Journal of the Atmospheric Sciences 67.3 (2010): 673-693. © 2010 American Meteorological Society As Published http://dx.doi.org/10.1175/2009jas3130.1 Publisher American Meteorological Society Version Final published version Citable link http://hdl.handle.net/1721.1/60347 Terms of Use Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. MARCH 2010 Z A L U C H A E T A L . 673 An Analysis of the Effect of Topography on the Martian Hadley Cells ANGELA M. ZALUCHA AND R. ALAN PLUMB Massachusetts Institute of Technology, Cambridge, Massachusetts R. JOHN WILSON Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey (Manuscript received 4 March 2009, in final form 17 September 2009) ABSTRACT Previous work with Mars general circulation models (MGCMs) has shown that the north–south slope in Martian topography causes asymmetries in the Hadley cells at equinox and in the annual average. To quantitatively solve for the latitude of the dividing streamline and poleward boundaries of the cells, the Hadley cell model of Lindzen and Hou was modified to include topography. The model was thermally forced by Newtonian relaxation to an equilibrium temperature profile calculated with daily averaged solar forcing at constant season.
    [Show full text]
  • What Drives Glacial Cycles Combined
    From Imbrie and Imbrie 1979 Table of Contents Page Foreword ..............................................................................................................................1 Chapter 1. ............................................................................................................................4 Climate’s Pacemaker; Cyclic Changes in the Earth’s Orbit Chapter 2. ..........................................................................................................................20 Atmospheric CO2: The Link between Ocean Circulation and Ice Extent Chapter 3. ..........................................................................................................................36 Climate’s Punctuator: Millennial Reoganizations of Ocean Circulation Chapter 4. ..........................................................................................................................58 Ocean Reorganizations: The Driver of Climate Change on Both Orbital and Millennial Time Scales Chapter 5. ..........................................................................................................................90 Cause of the Cooling Ramp Chapter 6. ..........................................................................................................................96 Unresolved Questions Epilogue ...........................................................................................................................101 Acknowledgements ..........................................................................................................101
    [Show full text]
  • Hydrologic Impacts of Past Shifts of Earthls Thermal Equator Offer
    PERSPECTIVE Hydrologic impacts of past shifts of Earth’s thermal equator offer insight into those to be produced by fossil fuel CO2 Wallace S. Broeckera and Aaron E. Putnama,b,1 aLamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964; and bClimate Change Institute, University of Maine, Orono, ME 04469 Edited by John C. H. Chiang, University of California, Berkeley, CA, and accepted by the Editorial Board August 31, 2013 (received for review February 3, 2013) Major changes in global rainfall patterns accompanied a northward shift of Earth’s thermal equator at the onset of an abrupt climate change 14.6 kya. This northward pull of Earth’s wind and rain belts stemmed from disintegration of North Atlantic winter sea ice cover, which steepened the interhemispheric meridional temperature gradient. A southward migration of Earth’s thermal equator may have accompanied the more recent Medieval Warm to Little Ice Age climate transition in the Northern Hemisphere. As fossil fuel CO2 warms the planet, the continents of the Northern Hemisphere are expected to warm faster than the Southern Hemisphere oceans. Therefore, we predict that a northward shift of Earth’s thermal equator, initiated by an increased interhemispheric temperature contrast, may well produce hydrologic changes similar to those that occurred during past Northern Hemisphere warm periods. If so, the American West, the Middle East, and southern Amazonia will become drier, and monsoonal Asia, Venezuela, and equatorial Africa will become wetter. Additional paleoclimate data should be acquired and model simulations should be conducted to evaluate the reliability of this analog. hydroclimate | deglaciation | global warming | Intertropical Convergence Zone As Earth warms in response to the continu- Hemisphere.
    [Show full text]
  • Download File
    SCIENCE ADVANCES | RESEARCH ARTICLE CLIMATOLOGY 2017 © The Authors, some rights reserved; Human-induced changes in the distribution of rainfall exclusive licensee American Association 1,2 2 for the Advancement Aaron E. Putnam * and Wallace S. Broecker of Science. Distributed under a Creative ’ A likely consequence of global warming will be the redistribution of Earth s rain belts, affecting water availability Commons Attribution ’ for many of Earth s inhabitants. We consider three ways in which planetary warming might influence the global NonCommercial distribution of precipitation. The first possibility is that rainfall in the tropics will increase and that the subtropics License 4.0 (CC BY-NC). and mid-latitudes will become more arid. A second possibility is that Earth’s thermal equator, around which the planet’s rain belts and dry zones are organized, will migrate northward. This northward shift will be a consequence of the Northern Hemisphere, with its large continental area, warming faster than the Southern Hemisphere, with its large oceanic area. A third possibility is that both of these scenarios will play out simultaneously. We review paleoclimate evidence suggesting that (i) the middle latitudes were wetter during the last glacial maximum, (ii) a northward shift of the thermal equator attended the abrupt Bølling-Allerød climatic transition ~14.6 thousand years ago, and (iii) a southward shift occurred during the more recent Little Ice Age. We also inspect trends in seasonal surface heating between the hemispheres over the past several decades. From these clues, we predict that there will be a seasonally dependent response in rainfall patterns to global warming.
    [Show full text]
  • Chapter 10 EVOLUTION of the INDO-PACIFIC WARM POOL AND
    Chapter 10 EVOLUTION OF THE INDO-PACIFIC WARM POOL AND HADLEY-WALKER CIRCULATION SINCE THE LAST DEGLACIATION Michael K. Gagan1 and Lonnie G. Thompson2 1Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia 2Department of Geological Sciences and Byrd Polar Research Center, The Ohio State Uni- versity, 108 Scott Hall, 1090 Carmack Road, Columbus, Ohio 43210-1002, U.S.A. Abstract The Indo-Pacific warm pool (IPWP), East Pacific cold tongue, and deep overturning atmospheric Hadley (meridional) and Walker (zonal) circulations form a tightly coupled system. In this chapter, we explore the concept of the Hadley circulation as the fundamental driver of changes in this system, and examine its possible impact on global climates of the past. Recent modeling studies indicate that the Hadley circulation is sensitive to Milankovitch forcing, dominated by the precession cycle (22,000 years) in the tropics. It is well estab- lished that the increasing Northern Hemisphere summer insolation during the post-glacial transition enhanced northern summer mon- soon rainfall, particularly across the Asian landmass. Based on the results of modeling studies, it is probable that the northward asym- metry in tropical heating led to asymmetrical intensification of the Hadley circulation during the early Holocene. The response of the tropical ocean to the intensification of the Had- ley circulation is given by foraminiferal Mg/Ca and coral Sr/Ca sea surface temperature (SST) reconstructions, which show that ocean- atmosphere feedbacks drove the tropical Pacific into a westward- concentrated La Niña–like state (warming in the west, cooling in the east) between ~11,000 and ~4,000 years ago.
    [Show full text]
  • The Shape of Continents, Air-Sea Interaction, and the Rising Branch of the Hadley Circulation
    To appear in The Hadley Circulation: Past, Present and Future, H. F. Diaz and R. S. Bradley (Eds.), Kluwer Academic Publishers, Dordrecht. The Shape of Continents, Air-Sea Interaction, and the Rising Branch of the Hadley Circulation Shang-Ping Xie International Pacific Research Center and Department of Meteorology, University of Hawaii Honolulu, HI 96822, USA ([email protected]) This chapter begins with a brief history of ITCZ research, and then goes on to summarize the recent progress in understanding why the ITCZ is locked in the Northern Hemisphere in the eastern Pacific and Atlantic, and how this northward-displaced ITCZ affects the space- time structure of tropical climate variability. ___________________ 1. Introduction The rest of the chapter is organized as follows. Sections 2 and 3 give historical and observational background, The differential solar radiation in the meridional direction is respectively. Section 4 investigates ocean-atmosphere the ultimate drive for the global Hadley circulation, dictating interactions that maintain the climatic asymmetry of the that its rising branch and heavy rainfall should be located near northward-displaced ITCZ, and Section 5 considers the effect the equator. This solar forcing of the atmosphere is indirect, of land-sea distribution. Section 6 discusses the climatic however, since most of solar radiation absorption takes place consequence of the northward-displaced ITCZ. Following a at the surface of Earth. Over the tropical oceans, most of the discussion of some remaining issues in Section 7, Section 8 absorbed solar energy is used for surface evaporation and the summarizes the main results. resultant water vapor is gathered by winds to fuel deep convection that is organized into zonally oriented rain bands.
    [Show full text]