1. January History Great Flood of 1937 70% of Louisville was submerged 3.3 billion in damages Crest - 85.4 ft. (Flood Stage – 55 ft.) 15 inches of rain in 12 days

2. Chapter 1: Monitoring the Weather (Basics) One of the Deepest Extratropical Cyclones Ever Recorded

3. Difference between Weather and Climate Weather is the state of the atmosphere at some place and time – Described with quantitative variables Temperature, humidity, cloudiness, precipitation, wind speed, wind direction – Meteorology is the study of the atmosphere and the processes that cause weather Climate is weather conditions at some locality averaged over a specified time period – Climate is an average of the weather, figured over the last 30- years and updated every decade – A locale’s climate also includes weather extremes

4. Look at Climatological Information

5. Sources of Weather Information Television – The Weather Channel and local newscasts Radio – NOAA Weather Radio Continuous broadcasts repeated every 4 - 6 minutes Interrupted with warnings and watches The Internet (Ag Weather) What about now? Survey of Farmers at the 2013 National Farm Machinery Show

6. Retrieving Weather Information & Maps Weather info received via TV, radio, or the Internet includes – Weather maps National Regional – Satellite/radar images – Data on current/past conditions – Weather forecasts Short-term – 24 – 48 hours Long-term – Up to 7 days or longer

7. Two Types of Pressure Systems High Pressure Systems, or “Anticyclones” Low Pressure Systems, or “Cyclones”

8. Pressure Systems Cont. High and low refer to air pressure – High pressure area is relatively high compared to surrounding air – Low pressure area is relatively low compared to surrounding air Highs – Fair weather – Clockwise rotation of sinking air (in Northern Hemisphere) – Generally track toward the east and southeast Lows – Stormy weather – Counterclockwise rotation of rising air (in Northern Hemisphere) – Generally track toward the east and northeast – Lows tracking across the northern U.S. or southern Canada produce less moisture than lows tracking across the southern U.S. – Weather to the west and north – usually cold – Weather to the south and east – usually warm

9. Pressure Systems Cont. (High and Low Pressure Centers) Arrows indicate surface horizontal winds

10. Pressure Systems Cont. (What’s the weather like?) 1. Tallahassee, FL 2. Greenville, NC 3. Duluth, MN 4. Scranton, PA Wind Direction? Cloudy/Wet, Clear/Dry?

11. Air Masses Huge volume of air covering thousands of square kilometers Horizontally relatively uniform in characteristics – Temperature – Humidity Gathers characteristics from its source region – Cold, dry air masses form at higher latitudes over continents – Cold, humid air masses form at higher latitudes over maritime surfaces – Warm, dry air masses form over continents in subtropical regions – Warm, humid air masses form near the equator or in the subtropics over maritime surfaces

12. Air Masses Across North America Old Saying in the Ohio Valley: “Don’t like the weather today? It will change tomorrow!”

13. Fronts “Transition Zones between Air Masses” Warm Air Rising Warm Front Cold Front

14. Fronts – Boundary Between Air Masses 1.Cold Front a.Generally, a narrow band of precipitation along or just ahead of the surface front, where precipitation is brief (couple of minutes to a few hours) b.Precipitation can be severe c.Boundary between advancing cold air and retreating warm air d.Plotted on a map as a blue line with triangles pointed in the direction of motion e.Sharp Temperature Change

15. Fronts – Boundary Between Air Masses 2. Warm Front a.Generally, a wide band of precipitation along or just ahead of the surface warm front, where precipitation can be persistent (12-24 hours) b.Precipitation is generally light to moderate c.Boundary between advancing warm air and retreating cold air d.Plotted on a map as a red line with semi-circles pointed in the direction of motion

16. Fronts – Boundary Between Air Masses Right - A cyclone with the warm and cold fronts extending outward from the low pressure center. Showers generally form along the warm front, while more severe weather can occur along the cold front. Left - Shows how the warm and cold fronts act as boundaries between different air masses. Notice how the wind directions are different on either side of the fronts, and that the flow is counterclockwise and convergent.

17. Ways to Locate a Front on a Surface Weather Map 1.Precipitation 2.Cloud Cover 3.Wind Shift 4.Temperature Difference 5.Dew Point Difference

18. Other Types of Frontal Boundaries 1.Stationary – a non-moving front where winds on either side blow in opposite directions. Can become a cold or warm front based on advection. 2. Occluded – when the air behind the cold front overtakes the air ahead of the warm front

19. Characteristics of Air Masses & Fronts Wind directions are different on the two sides of a front Some fronts have no clouds or precipitation. Passage indicated by wind shift, and temperature/humidity changes In summer, temperature can be nearly the same on both sides of a cold front Difference will be humidity Fronts are anchored to lows on a weather map. Counterclockwise flow brings contrasting air masses together to form fronts Thunderstorms/severe weather often occur in the warm, humid air mass located between the cold and warm front

20. Describing the State of the Atmosphere What do Forecasters Tell Us? Maximum Temperature – Usually occurs in early to mid-afternoon Minimum temperature – Usually occurs around sunrise Dewpoint (frost point) – The temperature at which air must be cooled at constant pressure to become saturated with water vapor and for dew (or frost) to form Relative humidity – A percentage; the ratio of the actual concentration of the water vapor component of air compared to the concentration the air would have if saturated with water vapor Relative humidity will change throughout the day as the temperature varies Generally highest around sunrise and lowest when warmest Precipitation amounts – General rule – 10” of snow = 1” of precipitation

21. Example: What do forecasters tell us? Dew Point Temp FHuman PerceptionR. Humidity 75 +Extremely uncomfortable, oppressive62% 70-74Very Humid, quite uncomfortable52-60% 65-69Somewhat uncomfortable for most people44-52% 60-64OK for most37-46% 55-59Comfortable31-41% 50-54Very comfortable31-37% 49 or lowerFeels like the western US30% Livestock Cold Stress? None Danger Emergency

22. Describing the State of the Atmosphere Cont. What do Forecasters Tell Us? Air Pressure – And its tendency (rising or falling) – Falling may indicate approaching cold front Wind direction and speed – Wind direction is the direction wind is blowing from Example; a west wind is blowing from the west, toward the east Sky cover – Fraction of the sky covered in clouds NWS Weather watch – issued when hazardous weather is considered possible NWS Weather warning – issued when hazardous weather is imminent or actually taking place

23. Weather Satellite Imagery Two major types of satellite orbits – Geostationary High orbits – 36,000 km (22,300 miles) high Orbits planet at same rate as Earth’s rotation and in same eastward direction Currently 2 of these provide a complete view of much of N. America and adjacent oceans to latitudes of about 60 degrees – Positioned over equator at 75 0 W longitude, 135 0 W longitude – Low angle in polar regions – Polar orbiting Low orbits – 800-1000 km (~500-600 miles) high (Much more detailed info) Provides overlapping north-south strips of images Passes over the same point twice every 24 hours

24. Orbits of Each Type of Satellite Geostationary Satellite Polar Orbiting Satellite

25. Weather Satellite Imagery Visible Black and white photograph of the planet Only available during daylight hours Highly reflective surfaces appear bright white and less reflective surfaces are darker

26. Weather Satellite Imagery Infrared Available anytime, not just during daylight Provides temperature comparison of features within image Whiter = colder Higher cloud tops appear whiter, because they are colder

27. Weather Satellite Imagery Water vapor imagery Enables tracking of plumes of moisture Shades of white = increasing moisture Upper-level clouds appear milky to bright white

28. Weather Radar Complements satellite surveillance Doppler radar detects movement Excellent tool to forecast tornadoes

29. Sky Watching You can determine much about the weather by watching the sky Clouds are aggregates of tiny water droplets, ice crystals, or some combination of both – A cloud in contact with the ground is fog – Cloud forms: Stratiform clouds are sheet-like clouds formed in horizontal layers – Form where air ascends gradually over a broad region Cumuliform clouds are puffy, like cotton balls – More vigorous ascent of air over a smaller area – Under the right conditions can build vertically into a cumulonimbus (thunderstorm) cloud The appearance of high, wispy, feather-like clouds (composed of ice) in the western sky is often the first sign of an approaching warm front

30. Cloud Forms These high thin cirrus clouds appear fibrous because they are composed of mostly tiny ice crystals

31. Cloud Forms These relatively low clouds are composed of tiny water droplets and have more sharply defined edges than ice-crystal clouds

32. Clouds Forms Fog, stratus clouds in contact with the ground, reduces visibility

33. Cloud Forms Fair weather cumulus clouds are most common during the warmest time of day and then vaporize after sunset

34. Cloud Forms Clouds of vertical development – Merging and vertically-growing cumulus clouds Can become Cumulonimbus clouds – Nimbo, nimbus prefix or suffix = rain producing – These clouds always produce lightning and sometimes heavy rain, hail, or strong and gusty surface winds

35. Cloud Forms Clouds may move in different directions at different altitudes – Indicates horizontal wind shifts with altitude

36. Understanding UTC Time Weather observations are taken across the world based on a standard time. In doing so, a 24 hour clock is used, similar to military time. UTC (Coordinated Universal Time or Universal Time Coordinated) Also called “Z Time” To get local time in the United States, you have to subtract a certain number of hours based on time zone. Daylight Savings Time does make a difference

37. Understanding UTC Time UTC Time = 1200 UTC Daylight Savings Time? (Not until March 8 th ) No -5 Hours for EST = 7 AM 18 UTC = 18Z = ? 00 UTC = 0Z = ? 06 UTC = 6Z = ?