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Fire Weather: Winds WINDS: general rules • All winds blow in response to pressure differences: from high to low pressure • What factors create pressure differences? – Temperature differences: Heating or cooling – Pressure cells and fronts Surface weather map • Lines (isobars) through points of equal sea-level pressure • Outline areas of high and low pressure -Low-pressure centers: “Lows” -Line of low pressure: “Trough” -High-pressure area: “High” -Lines of high pressure: “Ridge” High and Low Pressure Cells Winds blow inward, lifting (convection) Winds blow outward, descending (subsidence) Counterclockwise direction Clockwise direction Cooling, increased RH Warming, may be very dry air Can produce condensation, clouds, rain Few clouds, little or no rain General Winds • Gradient winds – Undisturbed by the topography of the earth Local Winds • = small-scale winds caused by local temperature (and pressure) differences • Affected by the topography and surface of the Earth Local Winds: General Rules • • • • • Warm air – rises or sinks? Cool air – rises or sinks? Cool, moist air = high or low pressure? Warm, dry air = high or low pressure? Heating of land vs. water – which heats faster? • Air temperature change between night and day? TTYP You will receive a picture of one of the following types of local winds. Develop a definition (in your own words) of the processes that cause that wind to blow. How do you think that particular wind will affect fire behavior? • Sea breeze – land breeze • Slope wind • Valley wind • Foehn wind • Turbulence • Thunderstorm drafts Sea Breeze – Land Breeze Sea Breeze – Land Breeze • Heating of land surface greater than water (water – high conductance/transparency) • Low pressure over land • Cool, moist air (high pressure) flows from sea to land • Nighttime: Land surface cools more quickly than water surface – reverse circulation • Wind speeds greater for sea breeze than for land breeze Slope Winds Slope Wind • Upslope winds – day – Heating of surface air • Downslope winds – night – Cooling of surface air – Cooled dense air falls (gravity) – Usually not as strong as upslope winds Valley Winds Valley Winds • Air in valleys becomes warmer than adjacent plains • Creates pressure gradient (lower pressure in valley) = upvalley winds • Begin late morning or early afternoon (most air warmed) • Downvalley winds = early night – cool, heavy air sinks Foehn Winds Foehn (“fern”) Winds • • • • Mountain systems Warm and dry downflowing wind Creates critical fire-weather situations Three forces: – Gravity – cool, heavy air descends down leeward side – Compression – descending air on leeward side = warm, dry – Pressure gradient – different pressures on either side of the mountain moves lower pressure air away from lee-side (replaced by warm foehn) Turbulence Turbulence • Mechanical turbulence – surface friction – Mountain waves – Eddies (lee side of trees, canyons) – Tree canopies • Thermal turbulence - intense local heating & convection – Whirlwinds, dust devils, firewhirls Thunderstorm drafts Fire Weather: Air Masses and Fronts Air Mass • Body of air having uniform characteristics – Temperature – Humidity • Acquire characteristics of source region Classification of air masses • • • • “P” = polar “T” = tropical “m” = maritime “c” = continental Polar – coldness Tropics – heat Oceans – moisture Continents - dryness Fronts • What is a “front”? – Two air masses meet • Different densities (don’t mix) • Surface of contact = “front” • What happens when warm and cold air meet? What are the possible effects on fire behavior? – – – – Gusty winds Turbulence Lightning & storms Dry air Fronts formed in troughs of low pressure Cold front • Cold air replaces warm air • Faster moving, steeper slope • High temperature gradient Cold front: wind shifts • • • • • Winds ahead of front S/SW Winds shift 45 – 180 degrees – from W NW N Wind change sharp and distinct Winds often gusty, unstable air Squall lines – line of showers & T-storms Effect of cold fronts on fire? • Severe fire weather • Especially dry cold fronts Warm Front • warm air replaces cold air • flat surface = clouds and rain spread out Warm front: Wind shifts • Winds ahead of front SE/S shift to SW • Change in wind direction 45-90 degrees – clockwise direction (N hemisphere) • Steady winds before and after frontal passage (air next to ground stable) Effect of warm fronts on fire? • Fire weather often positive • Moist air and steady rain Stationary Front • Forces on 2 air masses similar – little movement • Surface winds blow parallel to front, in opposite directions • Weather: similar to warm front, less intense • May quickly change to moving fronts Occluded Front • Cold front moves faster than warm front – overtakes it – warm air forced aloft between 2 cold fronts Occluded fronts: wind shifts • Wind shift usually > 90 degrees • Winds shift from S to W or NW • Weather: cloudiness and rain (severity depends on temperatures of fronts)