Lesson 2 C Weather 2 C1 S 190

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Lesson 2 C - Weather 2 C-1 -S 190 -EP

Lesson 2 C - Weather 2 C-1 -S 190 -EP

Lesson Objectives 1. Describe the affect of temperature and relative humidity has on wildland

Lesson Objectives 1. Describe the affect of temperature and relative humidity has on wildland fire behavior. 2. Describe the affect of precipitation on wildland fire behavior. 3. Describe the differences between a stable and unstable atmosphere. 4. Describe general and local winds. 5. Describe critical fire weather conditions. 6. List the different types of fire weather forecasts and outlooks available. 2 C-2 -S 190 -EP

Fire Weather *Click on image to play video 2 C-3 -S 190 -EP

Fire Weather *Click on image to play video 2 C-3 -S 190 -EP

Air Temperature The degree of hotness or coldness of a substance. An average of

Air Temperature The degree of hotness or coldness of a substance. An average of thermal energy of a group of particles in a substance (does not depend on # of particles) In weather we refer to this as air temperature or dry bulb temperature. 2 C-4 -S 190 -EP

Temperature is measured with a thermometer calibrated either to the FAHRENHEIT scale or the

Temperature is measured with a thermometer calibrated either to the FAHRENHEIT scale or the CELSIUS or centigrade scale. What influences air temperature? • Time of day • Season • Elevation • Topography • Latitude • Weather systems • Bodies of water Why does air temperature matter in wildland fires? 2 C-5 -S 190 -EP

Relative Humidity For a given air temperature, relative humidity (%) is the amount of

Relative Humidity For a given air temperature, relative humidity (%) is the amount of moisture in the air divided by the amount the air could hold when saturated; usually expressed in percent. • Ranges from 1 -100%. . . what does 100% mean? 2 C-6 -S 190 -EP

Temperature and RH Relationships 3 grams of H 2 O 50ºF 100% (saturated) 70ºF

Temperature and RH Relationships 3 grams of H 2 O 50ºF 100% (saturated) 70ºF 50% (unsaturated) 90ºF 25% (unsaturated) 2 C-7 -S 190 -EP

Thermograph Temperature and RH Relationship 2 C-8 -S 190 -EP

Thermograph Temperature and RH Relationship 2 C-8 -S 190 -EP

Relative Humidity Temperature vs. RH (general) for a given volume of air A Temp.

Relative Humidity Temperature vs. RH (general) for a given volume of air A Temp. = 60 F RH = X B Temp. = 80 F RH = X/2 Temperature 2 C-9 -S 190 -EP

So what? • Think of the fire triangles…what does RH affect? – Does this

So what? • Think of the fire triangles…what does RH affect? – Does this differ between fine/large fuels? • Why does this matter for wildland fire suppression? • Why does this matter for prescribed burning? – Small changes in RH that aren’t noticed can have significant impacts • What should you do on a fire? • Monitoring = belt weather kit 2 C-10 -S 190 -EP

Precipitation is liquid or solid water particles that originate in the atmosphere, and become

Precipitation is liquid or solid water particles that originate in the atmosphere, and become large enough to fall to the earth’s surface. 2 C-11 -S 190 -EP

Precipitation Amount vs. Duration • Fine Fuels – gain and lose moisture quickly –

Precipitation Amount vs. Duration • Fine Fuels – gain and lose moisture quickly – react rapidly to precipitation • Heavy Fuels – gain and lose moisture slowly – react slowly to precipitation • Duration vs. Amount – Precipitation duration has greater impact on fuel moisture than precipitation amount 2 C-12 -S 190 -EP

Atmospheric Stability The degree to which vertical motion in the atmosphere is ENHANCED or

Atmospheric Stability The degree to which vertical motion in the atmosphere is ENHANCED or SUPPRESSED. *Click on image to play video 2 C-13 -S 190 -EP

Stable Atmosphere Stable atmosphere resists upward vertical motion *Click on image to play video

Stable Atmosphere Stable atmosphere resists upward vertical motion *Click on image to play video 2 C-14 -S 190 -EP

Stable Atmosphere Visual Indicators • Visual Indicators – Clouds form in layers – Smoke

Stable Atmosphere Visual Indicators • Visual Indicators – Clouds form in layers – Smoke drifts apart after limited rise – Poor visibility due to smoke or haze – Fog layers – Steady winds 2 C-15 -S 190 -EP

Stable Atmosphere Visual Indicator Examples • Clouds form in layers 2 C-16 -S 190

Stable Atmosphere Visual Indicator Examples • Clouds form in layers 2 C-16 -S 190 -EP

Stable Atmosphere Visual Indicator Examples • Smoke drifts apart after limited rise 2 C-17

Stable Atmosphere Visual Indicator Examples • Smoke drifts apart after limited rise 2 C-17 -S 190 -EP

Stable Atmosphere Visual Indicator Examples • Poor visibility due to smoke or haze 2

Stable Atmosphere Visual Indicator Examples • Poor visibility due to smoke or haze 2 C-18 -S 190 -EP

Stable Atmosphere Visual Indicator Examples • Fog Layers 2 C-19 -S 190 -EP

Stable Atmosphere Visual Indicator Examples • Fog Layers 2 C-19 -S 190 -EP

Stable Atmosphere Visual Indicator Examples • Steady Winds 2 C-20 -S 190 -EP

Stable Atmosphere Visual Indicator Examples • Steady Winds 2 C-20 -S 190 -EP

Stable Atmosphere Inversion *Click on image to play video 2 C-21 -S 190 -EP

Stable Atmosphere Inversion *Click on image to play video 2 C-21 -S 190 -EP

Stable Atmosphere Inversion Types • Four Inversion Types – – Nighttime (Radiation) Frontal Marine

Stable Atmosphere Inversion Types • Four Inversion Types – – Nighttime (Radiation) Frontal Marine Subsidence • Two most common types – Nighttime (Radiation) – Subsidence 2 C-22 -S 190 -EP

Stable Atmosphere Nighttime Inversion *Click on image to play video 2 C-23 -S 190

Stable Atmosphere Nighttime Inversion *Click on image to play video 2 C-23 -S 190 -EP

Stable Atmosphere Thermal Belt • Thermal Belt – Nighttime inversions in mountainous regions –

Stable Atmosphere Thermal Belt • Thermal Belt – Nighttime inversions in mountainous regions – The warm layer typically found on the middle third of the slope – Characterized by the highest minimum temperature and lowest minimum RH – Fire can be very active within thermal belt 2 C-24 -S 190 -EP

Stable Atmosphere Subsidence Inversion *Click on image to play video 2 C-25 -S 190

Stable Atmosphere Subsidence Inversion *Click on image to play video 2 C-25 -S 190 -EP

Stable Atmosphere Subsidence Inversion Facts • Subsidence Inversion – May persist for several days

Stable Atmosphere Subsidence Inversion Facts • Subsidence Inversion – May persist for several days – May reach the surface further enhancing fire activity – Typically results in • clear or cloudless skies • above average temperatures • low relative humidity • drying of fuels 2 C-26 -S 190 -EP

Unstable Atmosphere Encouraging upward vertical motion 2 C-27 -S 190 -EP

Unstable Atmosphere Encouraging upward vertical motion 2 C-27 -S 190 -EP

Unstable Atmosphere Visual Indicators • Visual Indicators – Clouds grow vertically and smoke rises

Unstable Atmosphere Visual Indicators • Visual Indicators – Clouds grow vertically and smoke rises to great heights – Cumulus clouds – Good visibility – Gusty winds – Dust devils and firewhirls 2 C-28 -S 190 -EP

Unstable Atmosphere Visual Indicator Examples • Clouds grow vertically and smoke rises to great

Unstable Atmosphere Visual Indicator Examples • Clouds grow vertically and smoke rises to great heights 2 C-29 -S 190 -EP

Unstable Atmosphere Visual Indicator Examples • Cumulus Clouds • Good Visibility 2 C-30 -S

Unstable Atmosphere Visual Indicator Examples • Cumulus Clouds • Good Visibility 2 C-30 -S 190 -EP

Unstable Atmosphere Visual Indicator Examples • Gusty Winds • Dust devils and firewhirls *Click

Unstable Atmosphere Visual Indicator Examples • Gusty Winds • Dust devils and firewhirls *Click on image to play video 2 C-31 -S 190 -EP

Winds Horizontal movement of air *Click on image to play video 2 C-32 -S

Winds Horizontal movement of air *Click on image to play video 2 C-32 -S 190 -EP

Winds Wind’s Effect on Wildland Fire • Wind impacts the fire environment by: –

Winds Wind’s Effect on Wildland Fire • Wind impacts the fire environment by: – – Increasing the supply of oxygen to the fire. Determining the direction of fire spread. Increasing the drying of the fuels. Carrying sparks and firebrands ahead of the main fire causing new spot fires. – Bending flames, which results in the preheating of fuels ahead of the fire. – Influencing the amount of fuel consumed by affecting the residence time of the flaming front of the fire. The stronger the wind, the shorter the residence time and the less fuel is consumed. 2 C-33 -S 190 -EP

General Winds *Click on image to play video 2 C-34 -S 190 -EP

General Winds *Click on image to play video 2 C-34 -S 190 -EP

Local Winds *Click on image to play video 2 C-35 -S 190 -EP

Local Winds *Click on image to play video 2 C-35 -S 190 -EP

Local Winds Slope Winds • Upslope Winds – A result of differential heating and

Local Winds Slope Winds • Upslope Winds – A result of differential heating and convective processes along the slope – Average speeds range from 3 to 8 mph – Develop along east facing slope first and south and west facing slope by late morning • Downslope Winds – Air along the slope cools and sinks producing the downslope wind – Average speeds range from 2 to 5 mph – Develop on east facing aspects first and south and west facing aspects after sunset 2 C-36 -S 190 -EP

Local Winds Valley Winds • Upvalley Winds – As the air warm, temperature and

Local Winds Valley Winds • Upvalley Winds – As the air warm, temperature and pressure differences within the valley or adjacent valleys result in upvalley wind flow. – Strongest mid to late afternoon. – Average speeds range from 10 to 15 mph. • Downvalley Winds – As the valley loses solar heating, the air in the valley cools. – The cool air drains downvalley. – Average downvalley wind speeds range from 5 to 10 mph. – Typically develop a few hours after sunset. 2 C-37 -S 190 -EP

Local Winds Sea/Land Breeze 2 C-38 -S 190 -EP

Local Winds Sea/Land Breeze 2 C-38 -S 190 -EP

Sea Breeze 1998 Perry Fire Sea breeze interacting with Perry fire. Fire activity increases

Sea Breeze 1998 Perry Fire Sea breeze interacting with Perry fire. Fire activity increases when sea breeze front penetrates fire. 2 C-39 -S 190 -EP

Used in Rx prescriptions • • • LVORI- Low Visibility Occurrence Risk Index “Smog”

Used in Rx prescriptions • • • LVORI- Low Visibility Occurrence Risk Index “Smog” index- risk of low visibility (vehicles) Increases with RH, and low DI – From operational experience, one should be VERY CAUTIOUS ABOUT BURNING if one of the following situations occurs: – When LVORI for a nighttime forecast period is 8, 9 or 10 – When ACTIVE SMOKE from stumps logs, etc. is present during the night – When there is a roadway within three miles of a burn site with open fields, logging roads, or open streams that can provide an easy transit of the smoke from the burn site to the roadway 2 C-40 -S 190 -EP

Used in Rx prescriptions • Dispersion Index – Estimates daytime and nightime stability of

Used in Rx prescriptions • Dispersion Index – Estimates daytime and nightime stability of the atmosphere. Higher DI = greater mixing, but very high = potential fire control problems – Doubling of the DI results in a doubling of the amount of smoke the airshed can hold – RX : 41 -70 – Under 30, could be OK…if small unit with little smoke, or stagnant if winds are low – Over 71: very good dispersion…but hazardous to burn 2 C-41 -S 190 -EP

Those who know how to read and heed weather! Those who think they can

Those who know how to read and heed weather! Those who think they can “weather it all” 2 C-42 -S 190 -EP

2008 burn Winter Annual ACMF 2 C-43 -S 190 -EP

2008 burn Winter Annual ACMF 2 C-43 -S 190 -EP

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2 C-44 -S 190 -EP

2 C-45 -S 190 -EP

2 C-45 -S 190 -EP

2 C-46 -S 190 -EP

2 C-46 -S 190 -EP

Review Lesson Objectives 1. Describe the affect of temperature and relative humidity has on

Review Lesson Objectives 1. Describe the affect of temperature and relative humidity has on wildland fire behavior. 2. Describe the affect of precipitation on wildland fire behavior. 3. Describe the differences between a stable and unstable atmosphere. 4. Describe general and local winds. 5. Describe critical fire weather conditions. 6. List the different types of fire weather forecasts and outlooks available. 2 C-47 -S 190 -EP

Critical Fire Weather *Click on image to play video 2 C-48 -S 190 -EP

Critical Fire Weather *Click on image to play video 2 C-48 -S 190 -EP

Critical Fire Weather Cold Fronts *Click on image to play video 2 C-49 -S

Critical Fire Weather Cold Fronts *Click on image to play video 2 C-49 -S 190 -EP

Critical Fire Weather Foehn Winds *Click on image to play video 2 C-50 -S

Critical Fire Weather Foehn Winds *Click on image to play video 2 C-50 -S 190 -EP

 • • • Meteorology Santa Ana winds are a type of drainage wind,

• • • Meteorology Santa Ana winds are a type of drainage wind, an offshore wind that results from the buildup of air pressure in the high-altitude Great Basin between the Sierra Nevada and the Rocky Mountains. When upper level winds are favorable, this high altitude air mass spills out of the Great Basin and is propelled gravitationally towards the southern California coastline, generally as a northeasterly wind. It is often said that the air is heated and dried as it passes through the Mojave and Sonoran deserts, but according to meteorologists this is a popular misconception. The Santa Ana winds usually form during autumn and early spring when the surface air in the elevated regions of the Great Basin and Mojave Desert (the "high desert") becomes cool or even cold, although they may form at virtually any time of year. The air heats up due to adiabatic heating during its descent. While the air has already been dried by orographic lift before reaching the Great Basin as well as by subsidence from the upper atmosphere, the relative humidity of the air is further decreased as it descends from the high desert toward the coast, often falling below 10 percent. The air from the high desert is initially relatively dense owing to its coolness and aridity, and thus tends to channel down the valleys and canyons in gusts which can attain hurricane force at times. As it descends, the air not only becomes drier, but also warms adiabatically by compression. The southern California coastal region gets some of its hottest weather of the year during autumn while Santa Ana winds are blowing. During Santa Ana conditions it is typically hotter along the coast than in the deserts. Quik. SCAT image showing the speed of the Santa Ana winds (m/s). Note that while the Santa Ana Winds are an adiabatic wind, they are not a Föhn wind. A Föhn wind results from precipitation on the windward side of a mountain range which releases latent heat into the atmosphere which is then warmer on the leeward side (e. g. the Chinook or the original Föhn). The Santa Ana winds do not originate in precipitation, but in the bone-dry high deserts. The combination of wind, heat, and dryness accompanying the Santa Ana winds turns the chaparral into explosive fuel feeding the infamous wildfires for which the region is known. Wildfires fanned by Santa Ana winds burned 721, 791 acres (2, 921 km²) in two weeks during October 2003. [1] These same winds have contributed to the fires that have burned some 426, 000 acres (1, 720 km 2) as of late October 2007. [2] Although the winds often have a destructive nature, they have some positive benefits as well. They cause cold water to rise from below the surface layer of the ocean, bringing with it many nutrients that ultimately benefit local fisheries. As the winds blow over the ocean, sea surface temperatures drop about 4°C (7°F), indicating the upwelling. Chlorophyll concentrations in the surface water go from negligible, in the absence of winds, to very active at more than 1. 5 milligrams per cubic meter in the presence of the winds. 2 C-51 -S 190 -EP

Critical Fire Weather Foehn Winds • Common Foehn Winds – Chinook – Wasatch –

Critical Fire Weather Foehn Winds • Common Foehn Winds – Chinook – Wasatch – North – East – Santa Ana 2 C-52 -S 190 -EP

San Diego, Oct. 2007 Californias love the Santa Ana winds 2 C-53 -S 190

San Diego, Oct. 2007 Californias love the Santa Ana winds 2 C-53 -S 190 -EP

Critical Fire Weather Thunderstorms 2 C-54 -S 190 -EP

Critical Fire Weather Thunderstorms 2 C-54 -S 190 -EP

Critical Fire Weather Dust Devils and Firewhirls *Click on image to play video 2

Critical Fire Weather Dust Devils and Firewhirls *Click on image to play video 2 C-55 -S 190 -EP

Complete Exercise 4 2 C-56 -S 190 -EP

Complete Exercise 4 2 C-56 -S 190 -EP

Predictive Services • Predictive Services – Products Produce By: • Agency Fire Meteorologists •

Predictive Services • Predictive Services – Products Produce By: • Agency Fire Meteorologists • Intelligence Coordinator • FBAN • Fuels Specialists – Monitors, analyzes and predicts • Fire weather • Fire danger • Interagency fire management resource impact 2 C-57 -S 190 -EP

Predictive Services (national, regional websites) • Predictive Services – 7 Day Significant Fire Potential

Predictive Services (national, regional websites) • Predictive Services – 7 Day Significant Fire Potential • Produced Weekly • Daily in 2006 – 30 Day Fire Potential • Produced Monthly – Season Fire Potential • Produced Annually – Spring – Fire Season Update • Southern Area Coordination Center 2 C-58 -S 190 -EP

DOF Website: http: //www. fldof. com/fire_weather/forecast/seasonal_forecast. html Seasonal Fire Weather Outlook: Updated January 4,

DOF Website: http: //www. fldof. com/fire_weather/forecast/seasonal_forecast. html Seasonal Fire Weather Outlook: Updated January 4, 2008 January-March 2008 • Current Conditions Around Florida: • The state began 2007 under neutral ENSO conditions but La Niña conditions formed later in the year. Dry conditions persisted through the fall due to the La Niña and positive Pacific North American (PNA) pattern…According to the U. S. Drought Monitor, most of the state is experiencing abnormally dry conditions with the south central part of the state seeing moderate to severe drought conditions. • Long-range Outlook: • The outlook for the next three months is for the current La Niña pattern to continue. Drought conditions are expected to worsen…Rainfall amounts are forecast to be near average by June and above average toward the end of the summer when we approach peak hurricane season. Summary: • Drought conditions are expected to worsen over the spring months as the La Niña in the eastern Pacific Ocean persists. The potential will be high for another active wildfire season this spring once again. Longer term outlooks suggest summer rainfall could be influenced by another active hurricane season. • The next forecast will be the first week in April, 2008. Should there be any questions, please contact Deborah Hanley at hanleyd@doacs. state. fl. us. 2 C-59 -S 190 -EP

National Weather Service • National Weather Service – Products produced for: • Fire Weather

National Weather Service • National Weather Service – Products produced for: • Fire Weather Zones – Products produced by: • Meteorologists – Products geared toward: • Tactical planning 2 C-60 -S 190 -EP

NWS: Fire Weather Planning Forecast FNUS 52 KJAX 171939 FWFJAXFIRE WEATHER PLANNING FORECAST FOR

NWS: Fire Weather Planning Forecast FNUS 52 KJAX 171939 FWFJAXFIRE WEATHER PLANNING FORECAST FOR NORTHEAST FLORIDA/SOUTHEAST GEORGIANATIONAL WEATHER SERVICE JACKSONVILLE FL 239 PM EST THU JAN 17 2008 DISCUSSION. . . • A narrative or tabular zone-type product • Here, will most likely be for JAX • Elements include: – Sky/weather – Temperature – Relative humidity LOW PRESSURE WILL TRACK ACROSS THE FORECAST AREATHIS EVENING AND PUSH NORTHEAST OF THE REGION TONIGHT. SCATTEREDSHOWERS WILL DISSIPATE THROUGH THE EVENING HOURS. WEAK HIGH PRESSUREWILL BUILD INTO THE REGION ON FRIDAY. ANOTHER LOW WILL DEVELOP INTHE GULF OF MEXICO SATURDAY AND TRACK NORTHEAST OF THE REGIONSETTING THE STAGE FOR A COLD. . . BRISK AND DRY SUNDAY WITH HIGHPRESSURE SETTING UP OVER THE REGION EARLY NEXT WEEK. RELATIVE HUMIDITIES WILL REMAIN ABOVE CRITICAL LEVELS THROUGH THE PERIODEXCEPT FOR SUNDAY WHEN RH VALUES WILL BOTTOM OUT IN THE 15 -25 PERCENTRANGE OVER THE INLAND SECTIONS AND RED FLAG WARNINGS MAY BE REQUIRED. WINDS LESS THAN 15 MPH ARE EXPECTED ON FRIDAY. NORTHWEST WINDS OF 15 TO 20 MPH ARE EXPECTED ON SATURDAY. NORTH WINDS OF 15 TO 20 MPHARE EXPECTED ON SUNDAY. NORTHEAST WINDS OF 15 TO 20 MPH WILLCONTINUE ON MONDAY AND SLOWLY DECREASE TO LESS THAN 15 MPH ONTUESDAY AND WEDNESDAY. GAZ 153 -154 -165 -166 -181045 -INLAND GLYNN-COASTAL GLYNN-INLAND CAMDEN-COASTAL CAMDEN-239 PM EST THU JAN 17 2008 TONIGHT FRI NIGHT SATCLOUD COVER PCLDY MCLDYCHANCE PRECIP (%) 0 0 80 WEATHER TYPE NONE SHOWERSTEMP 43 59 45 55 RH (%) 97 60 100 7020 FT WND MPH (AM) N 6 N 8 G 2120 FT WND MPH (PM) NW 8 N 4 NE 4 NW 14 G 26 PRECIP DURATION 11 PRECIP BEGIN 7 PM CONTINUINGPRECIP END 7 AM CONTINUINGPRECIP AMOUNT 0. 00 0. 69 0. 87 LAL 1 1 MIXING HEIGHT(FT-AGL) 500 2200 400 1600 TRANSPORT WND (MPH) N 13 N 7 NE 7 NW 30 DISPERSION INDEX 7 15 5 27 MAX LVORI 6 9 REMARKS. . . NONE. . FORECAST FOR DAYS 3 THROUGH 7. . SUNDAY. . . PARTLY CLOUDY. A 20 PERCENT CHANCE OF RAIN SHOWERS. LOWS IN THE UPPER 20 S. HIGHS IN THE LOWER 50 S. NORTHEAST WINDS 15 TO 20 MPH. . MONDAY. . . PARTLY CLOUDY. LOWS IN THE LOWER 30 S. HIGHS IN THEUPPER 50 S. NORTHEAST WINDS 10 TO 15 MPH. . TUESDAY. . . MOSTLY CLOUDY. A 50 PERCENT CHANCE OF RAIN SHOWERS. LOWS IN THE MID 40 S. HIGHS IN THE LOWER 60 S. EAST WINDS 5 TO 10 MPH. . WEDNESDAY THROUGH THURSDAY. . . MOSTLY CLOUDY WITH A 50 PERCENTCHANCE OF RAIN SHOWERS. LOWS IN THE LOWER 50 S. HIGHS IN THE UPPER 60 S. SOUTHWEST WINDS 5 TO 15 MPH. 2 C-61 -S 190 -EP

NWS: Fire Weather Watches / Red Flag Warnings • Issued when the combination of

NWS: Fire Weather Watches / Red Flag Warnings • Issued when the combination of dry fuels and weather conditions support extreme fire behavior or ignition is occurring or expected to occur. • Can prevent prescribed burning 2 C-62 -S 190 -EP

Fire Weather Watches • Issued when there is a high potential for the development

Fire Weather Watches • Issued when there is a high potential for the development of a Red Flag Event. • Normally issued 24 to 72 hours in advance. FIRE WEATHER WATCH NATIONAL WEATHER SERVICE MIDLAND/ODESSA TX 946 AM CST FRI JAN 27 2006. . . FIRE WEATHER WATCH IN EFFECT SATURDAY FOR THE GUADALUPE MOUNTAINS FOR RELATIVE HUMIDITIES OF 15 PERCENT OR LESS. . . SUSTAINED 20 FOOT WINDS OF 20 MPH OR GREATER AND HIGH FIRE DANGER. . . 2 C-63 -S 190 -EP

Red Flag Warnings • Used to warn of an impending, or occurring Red Flag

Red Flag Warnings • Used to warn of an impending, or occurring Red Flag event. Red Flag Warning/Fire Weather Watch Information. . . RED FLAG WARNING IN EFFECT ACROSS THE SUWANNEE VALLEY REGION OF NORTH FLORIDA FROM NOON TO 5 PM EST THIS AFTERNOON FOR LONG DURATIONS OF LOW RELATIVE HUMIDITY. . . 2 C-64 -S 190 -EP

Spot Weather Forecast– DOF in Florida– must have local information and location Florida Division

Spot Weather Forecast– DOF in Florida– must have local information and location Florida Division of Forestry - Spot Forecast ID: 1185873416 Date Issued: Tue Jul 31, 2007 at 05: 16 Name: Leda Kobziar Company: University of Florida Location: 29. 74 / -82. 21 • Site specific forecasts that are issued to fit time, topography and weather of a specific location. Forecast Time Temp Humidity Wind Speed Direction Cloud Cover Precip 5: 00 76 -79 85 -90% 3 -6 WNW BK 6: 00 77 -80 84 -89% 3 -6 WNW BK 7: 00 77 -80 83 -88% 4 -7 WNW BK 8: 00 78 -81 83 -88% 4 -7 WNW BK 9: 00 80 -83 78 -83% 4 -7 WNW BK 10: 00 82 -85 74 -79% 4 -7 WNW BK 11: 00 83 -86 70 -75% 4 -7 NW SC 12: 00 84 -87 68 -73% 4 -7 SSW SC 13: 00 85 -88 66 -71% 5 -8 ESE SC 12% Chance (Trace) 14: 00 86 -89 64 -69% 5 -8 N BK 15% Chance (Trace) BK 12% Chance (Trace) 15: 00 85 -88 65 -70% 5 -8 NNE 2 C-65 -S 190 -EP

Complete Exercise 5 2 C-66 -S 190 -EP

Complete Exercise 5 2 C-66 -S 190 -EP