Weather and Climate Basics
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1 Weather and Climate Basics Laura Boekel Forecaster at Bureau of Meteorology
2 Aims of this presentation To describe what I do as a forecaster at the Bureau of Meteorology To provide an interesting introduction to weather and climate To present examples of how theory relates to real-world forecasting
3 Forecasters at the Bureau Aviation forecasting Fire weather Public weather Severe weather Volcanic Ash Advisory Centre Tropical Cyclone Advisory Centre Climate Hydrology
4 Aviation Forecasting All of NT 24 hours Issue products and warnings Weather watch Hazards: Fog and low cloud, thunderstorms, turbulence.
5 Radio interviews Tweeting Take calls from the public Draw streamlines for NT news 7 day weather outlook Public Weather
6 Fire weather Use meteorological parameters to decide weather to issue a fire weather warning Temperatures Humidity Winds
7 Weather Basics
8 Weather Basics: Topics The atmosphere Air pressure Horizontal motion Vertical motion Cold fronts Tropical cyclones
9 Weather Basics: Topics The atmosphere Air pressure Horizontal motion Vertical motion Cold fronts Tropical cyclones
10 The Atmosphere
11 The Atmosphere Ozone absorption Where weather occurs
12 Weather Basics: Topics The atmosphere Air pressure Horizontal motion Vertical motion Cold fronts Tropical cyclones
13 Air Pressure Why is air pressure important in meteorology?
14 Air Pressure Force = mass X acceleration F=ma
15 Air Pressure Pressure: net force per unit area, P=F/A Air has mass Gravity pulls air down Air Pressure is the force exerted by the column of air directly above you. Measured by a barometer In millibars (mb) = hecto Pascals (hpa) = kg / ms 2 Sometimes inches of mercury
16 Air pressure and altitude If you are standing at the top of Mt Everest, will the air pressure be less or more then when you were standing at base camp?
17 Air pressure and altitude If air pressure is weight of air above you Then less air above you means lower air pressure
18 Air pressure and its importance How does air pressure relate to weather patterns? Horizontal motion Vertical motion
19 Weather Basics: Topics The atmosphere Air pressure Horizontal motion Vertical motion Cold fronts Tropical cyclones
20 Air pressure and weather patterns Horizontal motion
21 Horizontal Motion Low Pressure High Pressure = Pressure Gradient Force
22 Coriolis Effect US1ro
23 Horizontal Motion Low Pressure High Pressure = Pressure Gradient Force = Coriolis force
24 Horizontal motion L H L = Pressure Gradient Force
25 Horizontal motion L H L = Coriolis force = Pressure Gradient Force
26
27 Important things to remember about wind: 1. It's described (or named) using the direction it is coming from a) southeast winds are coming FROM the southeast. 2. Wind speed is constantly changing: a) Gusts are a short increase in wind speed The Bureau of Meteorology reports wind as a 10 minute mean of wind speed or direction. 3. On land wind is given in kilometres per hour On water we use knots (nautical miles per hour). a) 1 knot = 1.85 km/h Wind gusts are the highest instantaneous wind speed measured within that 10 minute mean
28 Basics: Highs and Lows In the Southern Hemisphere: Motion around a Low is Clockwise Motion around a High is Anticlockwise
29 What about the tropics?
30 Wind and Air Pressure We can draw the wind fields around the pressure systems to analyse the weather
31 Gradient wind analysis
32 Weather Basics: Topics The atmosphere Air pressure Horizontal motion Vertical motion Cold fronts Tropical cyclones
33 Air pressure and weather patterns Vertical motion Rising of air = Sinking of air =
34 Sea breeze
35 Air Rises, but as it rises it and
36 Convection The water vapour in the air will condense into water droplets that form a cloud and can eventually grow into raindrops and fall from the cloud as rain H L H
37 Basics: Highs and Lows Showers and storms Clear skies, fog or low cloud LOW (falling pressures) HIGH (rising pressures)
38 Where s the weather? What is a weather front and why don't we get them in the tropics?
39 Weather Basics: Topics The atmosphere Air pressure Horizontal motion Vertical motion Cold fronts Tropical cyclones
40 Frontal systems (simplified) A front is a boundary separating two air masses
41 N S
42 N S
43 N S
44 N S
45 A front is a boundary separating two air masses
46 Cold fronts and weather Cold fronts cause warm air to rise and cool. Cooler water vapour condenses into cloud and rain ground
47 Why don't we get fronts in the tropics? The temperatures is the mostly the same across the tropics so that air circulating a low does not develop boundaries and or fronts N Instead we get tropical lows & tropical cyclones. S
48 Weather Basics: Topics The atmosphere Air pressure Horizontal motion Vertical motion Cold fronts Tropical cyclones
49 What is a Tropical Cyclone? A low pressure system of tropical origin having organised convection and gales near the centre Eye Eye Wall Rain bands Gale-force winds (10 min mean) 63 km/h (34 knots) (more than half way around the centre and persisting for at least 6 hours)
50 Super Typhoon Noul Animated GIF: MP4 movie file:
51 Category 1 Strongest Gust (km/h) Average Maximum Wind (km/h) Central Pressure (hpa) Typical Effects < > 985 Negligible house damage. Damage to some crops, trees and caravans. Craft may drag moorings
52 Category 2 Strongest Gust (km/h) Average Maximum Wind (km/h) Central Pressure (hpa) Typical Effects Minor house damage. Significant damage to signs, trees and caravans. Heavy damage to some crops. Risk of power failure. Small craft may break moorings.
53 Category 3 Strongest Gust (km/h) Average Maximum Wind (km/h) Central Pressure (hpa) Typical Effects Some roof and structural damage. Some caravans destroyed. Power failures likely. (e.g. Winifred)
54 Category 4 Strongest Gust (km/h) Average Maximum Wind (km/h) Central Pressure (hpa) Typical Effects Significant roofing loss and structural damage. Many caravans destroyed and blown away. Dangerous airborne debris. Widespread power failures. (e.g. Tracy, Olivia)
55 Category 5 Strongest Gust (km/h) Average Maximum Wind (km/h) Central Pressure (hpa) Typical Effects > 279 > 200 < 930 Extremely dangerous with widespread destruction. (e.g. Vance)
56 Climatology Basics
57 Climatology Basics Definitions Global Energy Budget Global Circulation Monsoon
58 Climatology Basics Definitions Global Energy Budget Global Circulation Monsoon
59 What is the difference between weather and climate? Weather: The current state of the atmosphere the short-term (minutes to days) variations in the atmosphere AMS Glossary of Meteorology Climate: The slowly varying aspects of the atmosphere-hydrosphere-land surface system AMS Glossary of Meteorology The climate is what you expect, the weather is what you get
60 Climatology: average conditions and anomalies Climate: The slowly varying aspects of the atmosphere-hydrosphere-land surface system AMS Glossary of Meteorology Often taken as a 30 year average Climate variability: any variations of the atmosphere/ocean system around a mean state AMS Glossary of Meteorology Why are some years wetter than others? What drives changes from season to season? Climate Change: Any systematic change in the long-term statistics of climate elements sustained over several decades or longer AMS Glossary of Meteorology
61 Climatology Basics Definitions Global Energy Budget Global Circulation Monsoon
62 Global Energy Balance How much energy comes into the Earth's climate system from the sun and what happens to this energy Balance: Incoming energy = outgoing energy Energy in = shortwave radiation Sun Energy out = longwave radiation Earth's surface, atmosphere, ect
63
64 Why is this energy balance important to climate? Greenhouse effect
65 Greenhouse Effect
66 Climatology Basics Definitions Global Energy Budget Global Circulation Monsoon
67 Global Circulation Even though synoptic patterns (highs/lows) effect winds, there is also a global circulation occurring on a much larger scale.
68 Single Cell Model
69 Three cell Model
70 Trade winds How does global circulation South-easterly flow across the Northern Territory Brings dry air from central Australia How does this explain monsoons/wet season? effect Darwin?
71 Climatology Basics Definitions Global Energy Budget Global Circulation Monsoon
72 Definitions Wet Season: The wetter part of the year. Runs from 1 October to 30 April Monsoon: derived from the Arabic word "mausam", meaning season. It is used to describe the seasonal reversal of winds that occurs over parts of the tropics.
73
74
75 A typical wet season O N D J F M A Build-up period: Oct-Dec Hot, humid Isolated thunderstorms Monsoon: End of December through April Bursts of widespread rainfall 1-3 Week long breaks in the rain
76 Bureau of Meteorology Graduate program Prerequisites: A degree, with a major in a physical science or mathematics
77 Thank you for your time Questions? Feel free to
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