Презентация на тему "Before"

Презентация: Before
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Скачать презентацию (3.72 Мб). Тема: "Before". Содержит 30 слайдов. Посмотреть онлайн с анимацией. Загружена пользователем в 2021 году. Оценить. Быстрый поиск похожих материалов.

  • Формат
    pptx (powerpoint)
  • Количество слайдов
    30
  • Слова
    другое
  • Конспект
    Отсутствует

Содержание

  • Презентация: Before
    Слайд 1

    Before

    and After Visual design in action

  • Слайд 2

    Our Teaching Tasks (cont.)

    In addition, we give lecture about Meteorology to students who want to become either: Private Pilots Commercial Pilots Airline Transport Pilots Air Traffic Controllers Before

  • Слайд 3

    We also teach aviation students Private pilots Commercial pilots Air traffic controllers Airline transport pilots After

  • Слайд 4

    Climatic Changes and the BoQ

    4 of 14 Temperature Rises 0.4°-2.0°C across Australia by 2030 9-12 days above 35°C in Melbourne BoQ has only 3-4 per year Rainfall -10%-+5% variations in rainfall in SE Australia by 2030 Barwon Region water deficit will be 80% of today’s use by 2055 Stage 4 Restrictions most of last year Storm Surges coastal regions particularly vulnerable storm surges likely to increase BoQ faces Port Phillip Heads Before

  • Слайд 5

    Climate changes will affect our environment

    Sea level rise Temperature Rainfall 0.4-2.0 C 9-12 days > 35 C (currently 3-4 days/year) Heat waves -10 - +5% Water restrictions Storm surges After

  • Слайд 6

    Students learning from the transformed slide scored higher on an identical test question

    Led to 54% correct Led to 86% correct Q: Heat source for movement of lithospheric plates? p

  • Слайд 7

    Topography

    ~20% Errors in old topography …and very smooth Before

  • Слайд 8

    The new model topography is 20% more accurate

    ~20% Errors in old topography …and very smooth Assertion as a sentence Evidence supporting assertion After

  • Слайд 9

    Superadiabatic Lapse Rates

    3/03/2021 9 Superadiabats are areas of the atmosphere where the temp-eraturedecreases with height at a faster rate than the dry adiabatic lapse rate Before

  • Слайд 10

    Superadiabats

    3/03/2021 10 Indicate an unstable atmosphere. Are either very important (meteorologically) or are spurious. Spurious superadiabats can be caused by: weak signals wet bulb effects. Spurious superadiabats should be eliminated from the sounding. Before

  • Слайд 11

    Temperatures in superadiabatic lapse rates decrease faster than dry adiabatic rates

    Unstable Important or Spurious Weak signal Wet bulb Eliminate After

  • Слайд 12

    12 Assumptions What is negotiation? Who is a negotiator? Why does it work? Why does it fail? How can we improve? A dozen tips… “Expanding the pie” Overview Before

  • Слайд 13

    Making it work better What is negotiation? Who negotiates? Why it works or fails “Expanding the pie” Negotiation is to close deals After

  • Слайд 14

    Technique 1: Animated Gif

    There are many free or shareware Gif Animator programs available. Images must be in .gif format Set the time each image is visible Select ‘animate once’ or ‘continuous’ according to your needs Before

  • Слайд 15

    Animate once or ‘forever’ according to your needs There are many free or shareware Gif Animator programs Images must be in .gif format Set the time each image is visible Gif Animators: http://en.softonic.com/search/gif-animator Order of images may be reversed After

  • Слайд 16

    weak shear—heavy precipitation falling near or through the updraft strong shear—precipitation does not greatly interfere with the updraft Before

  • Слайд 17

    weak shear = major effect Precipitation can interfere with updrafts Strong shear = little effect After

  • Слайд 18

    This project plan looked boring and unappealing. I applied basic design principles to it. Before

  • Слайд 19

    It is much easier to navigate and to see what is important. This looks really interesting. I’d like to read it. My boss You have, It’s the same document Me After

  • Слайд 20

    10 = 1 x Base1 + 0 x Base0 = 1x101 + 0x100 (1x10 + 0x1) 255 = 2x102 + 5x101 + 5x100 (2x100 + 5x10 + 5x1) Decimal Numbers Before

  • Слайд 21

    Decimal numbers use 10 as their base

    10 255 After

  • Слайд 22

    aerul tropical mai cald si mai usor aluneca deasupra celui continental polar, mai rece, care inainteaza la suprafata solului ascensiunea fortata a aerului cald deasupra celui rece condensare rapida a vaporilor de apa - nebulozitate pronuntata - precipitatii abundente - intensificari ale vantului Before

  • Слайд 23

    Aerul tropical mai caldsi mai usoralunecadeasupra celui continental polar, mai rece, care inainteaza la suprafatasolului ascensiunea fortata a aerului cald deasupra celui rece condensare rapida a vaporilor de apa nebulozitatepronuntata precipitatiiabundente intensificari ale vantului After

  • Слайд 24

    Before After Example of repetitionto signal new sections

  • Слайд 25

    Example of colour repetitionto signal and link sections

  • Слайд 26

    Example of repetition Sections Colours Fonts Positions Title and call-to-action slides

  • Слайд 27

    the storm containsa mesocyclon with an azimuthal velocity differential at base level > 7 m s-1, 2. storm persist for 30 min or greater, 3. cell initiation is based on first occurrence of a 40-dBZ echo, 4. termination is based on the loss of the mesocyclon. Criteria to select supercells storms Hocker, J.E., and J.B. Basara, 2008: A Geographic Information System-Based Analysis of Supercells across Oklahoma from 1994 to 2003. J. Appl. Meteor., 47, 1518–1538. Before

  • Слайд 28

    Criteria to select supercell storms Hocker, J.E., and J.B. Basara, 2008: A Geographic Information System-Based Analysis of Supercells across Oklahoma from 1994 to 2003. J. Appl. Meteor., 47, 1518–1538. Initiation Termination 40 dBZ echo Criteria no longer met Mesocyclone > 7 m s-1 at base level >= 30 minutes After

  • Слайд 29

    Diurnal variation Before

  • Слайд 30

    Most storms initiate between 3 and 9 PM 03 06 09 12 15 18 21 24 local After

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