Before and After Visual design in action

Before Our Teaching Tasks (cont. ) Ø In addition, we give lecture about Meteorology to students who want to become either: l l Private Pilots Commercial Pilots Airline Transport Pilots Air Traffic Controllers

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

Before Climatic Changes and the Bo. Q Temperature Rises • 0. 4°-2. 0°C across Australia by 2030 • 9 -12 days above 35°C in Melbourne • Bo. Q 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 • Bo. Q faces Port Phillip Heads 4 of 14

After Climate changes will affect our environment Temperature 0. 4 -2. 0 C Heat waves 9 -12 days > 35 C (currently 3 -4 days/year) Rainfall -10 - +5% Water restrictions Sea level rise Storm surges

Students learning from the transformed slide scored higher on an identical test question Q: Heat source for movement of lithospheric plates? Led to 54% correct p <. 001 Led to 86% correct These are results of tests of the assertion-evidence approach [Alley et al. , 2006]

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

The new model topography is 20% more accurate After Assertion as a sentence Evidence supporting assertion ~20% Errors in old topography …and very smooth

Before Superadiabatic Lapse Rates l 7/02/2018 Superadiabats areas of the atmosphere where the temperature decreases with height at a faster rate than the dry adiabatic lapse rate 9

Before Superadiabats Indicate an unstable atmosphere. l Are either very important (meteorologically) or are spurious. l Spurious superadiabats can be caused by: l l weak signals l wet bulb effects. l 7/02/2018 Spurious superadiabats should be eliminated from the sounding. 10

After Temperatures in superadiabatic lapse rates decrease faster than dry adiabatic rates Unstable Important or Spurious Weak signal Eliminate Wet bulb

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

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

Before 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

After Technique 1: Animated Gif There are many free or shareware Gif Animator programs Set the time each image is visible Images must be in. gif format Order of images may be reversed • Animate once or ‘forever’ according to your needs Gif Animators: http: //en. softonic. com/search/gif-animator

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

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

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

After 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

Before Decimal Numbers 10 = 1 x Base 1 + 0 x Base 0 = 1 x 101 + 0 x 100 (1 x 10 + 0 x 1) 255 = 2 x 102 + 5 x 101 + 5 x 100 (2 x 100 + 5 x 1)

After Decimal numbers use 10 as their base Base 1 1 10 255 Base 0 0 (101) (1 x 10 (100) + 0 x 1) Base 2 Base 1 Base 0 2 5 5 (102) 2 x 100 (101) + 5 x 10 (100) + 5 x 1

Before 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

After 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 Example of repetition to signal new sections After

Example of colour repetition to signal and link sections

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

Before Criteria to select supercells storms 1. the storm contains a 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 -d. BZ echo, 4. termination is based on the loss of the mesocyclon. 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.

After Criteria to select supercell storms Initiation >= 30 minutes Termination Mesocyclone > 7 m s-1 at base level 40 d. BZ echo Criteria no longer met 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 Diurnal variation

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