1/124
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai |
|---|
No analytics yet
Send a link to your students to track their progress
Heat
most fatalities of all severe weather in the US over the last 40 years
Heat Wave
a period of abnormally and uncomfortably hot and unusually humid weather, typically lasts two or more days
Heat Index
an accurate measure of how hot it really feels when relative humidity is added to the actual air temperature
Wet Bulb Globe Temperature
a parameter that estimates the effects of temperature, relative humidity, wind, and solar radiation on humans, good indicator of heat stress for active populations like outdoor workers and athletes
Extreme Heat Outlooks
issued when the potential exists for an excessive heat event in the next 3-7 days
Extreme Heat Watch
conditions are favorable for an excessive heat event in the next 24 to 72 hours, heat wave risk is increased but still uncertain
Heat Advisory
issued within 12 hours of the onset of dangerous heat conditions, 100 degrees or higher for at least two days and nighttime temps will not go below 75 degrees
Extreme Heat Warning
issued within 12 hours, max temperatures to be 105 degrees or higher for more than 3 hours per day for at least 2 days, nighttime temps will not go below 75 degrees
NWS HeatRisk Prototype
color-numeric based index that provides forecast risk of heat-related impacts, takes into account how unusual the heat is for the time of year, duration of heat, and if the temperatures pose an elevated risk of heat impacts, categories: Green → Yellow → Orange → Red → Magenta
Hyperthermia
body temperature above 40 degrees C (104 F)
Hyperthermia Warning Signs
high body temp, mental confusion, fainting, dry skin with rapid or slow pulse
Urban Heat Island
urban areas significantly warmer due to increased heat absorption, temperature difference larger at night, store more heat than rural areas
Heat and Air Pollution
heat waves can lead to poor air quality, increased ozone and particulate pollution
Changes in Heat Waves
frequency, duration, length of season, and intensity of heat waves have all gone up since the 1960s
Drought
period of abnormally dry weather long enough to cause a hydrologic imbalance in the affected area
Meteorological Drought
precipitation deficiency, reduced infiltration, high temp, greater sunshine, increased evaporation, and transpiration
Agricultural Drought
soil water deficiency, plant water stress, reduced biomass and yield
Hydrological drought
reduced streamflow, inflow to reservoirs, lakes, and ponds, reduced wetlands
Drought Characteristics
it is difficult to recognize, relative to normal amounts of water, government response to drought is lacking
What Causes Drought?
drought is a function of scale, and can be caused by various different things, like teleconnections, high pressure systems, climate change, or even human use of water
Why is Calculating Drought Hard?
finding the supply or the amount of rain and snow melt is easy, but the demand or evapotranspiration and soil moisture is more difficult to measure
Palmer Drought Severity Index
meteorological drought, uses precipitation, temp, and soil moisture to determine severity, does not take into account lag between precip and runoff/infiltration
Drought and Agriculture
U.S. farms contributed $164.7 billion to the economy, drought can cause crop failure and pasture losses and expand distribution of pests and diseases
Teleconnections
recurring and persistent, large-scale pattern of pressure and circulation anomalies that span vast geographical areas
ENSO
El Nino Southern Oscillation, fluctuation in sea surface temperatures (El Nino) and atmospheric pressure (Southern Oscillation), pressure differences between Darwin, Australia and Tahiti used to generate Southern Oscillation Index, lasts 6-18 months
Sustained Negative SOI Values
higher pressure than normal at Darwin, lower than normal at Tahiti, trade winds weaken, El Nino (warm phase)
Sustained Positive SOI Values
lower than normal pressure at Darwin, Higher than normal pressure at Tahiti, pacific trade winds strengthen, La Nina (cool phase)
El Nino
warm phase of ENSO (-SOI), five consecutive 3-month mean warmer than normal sea-surface temperatures in the eastern pacific, weaker trade winds, typically occurs around N.H. winter
La Nina
cool phase of ENSO (+SOI), five consecutive 3- month mean cooler than normal sea-surface temperatures in the eastern Pacific, stronger trade winds, upwelling on the Coast of South America
Jet Stream During El Nino
lower than usual, southern US experiences wet conditions, while northern US experiences warm and dry conditions
Jet Stream During El Nina
pushed northward, southern US experiences dry conditions, Pacific Northwest and Canada experience heavy rains
Fire
combination of oxygen with carbon, hydrogen, and other elements of organic material that produces flames, heat, and light
Fire Reaction
photosynthesis in reverse, oxygen combines with organic material, bonds between carbon and hydrogen are broke, chemical bonds form between carbon and oxygen and hydrogen and oxygen, energy given off as heat
Human Caused Fires
make up 85% of all fires
Natural Fires
make up 15% of all fires
Points of the Fire Behavior Triangle
fuels, topography, and weather
Weather
highest degree of variability in fire behavior triangle, high temperatures decrease moisture content in fuel source, low relative humidity increases risk for fires
Weather Elements that Influence Fire
stability: limits vertical transport of air
wind speed and direction: most important variable for spreading fire, hardest variable to predict
precipitation: increases relative humidity and adds to moisture content of fuels
Topography
most constant variable in fire behavior triangle
Topographic Features that Contribute to Fires
elevation: lowest ½ of slope is the hottest, upper ½ is the coldest
position on slope: know where the fire is located and where best fuels are present
aspect: direction a slope is facing
shape of terrain: can limit or enhance spread
steepness: stepper leads to greater heating and quicker spread, fire spreads most effectively uphill
Fuels
any combustible material, divided into four groups
Aerial Fuels
upper portion of trees, tree branches, tall shrubs
Ladder Fuels
surface fuel, small trees or shrubs, low branches, moss or lichen on tree trunks
Surface Fuels
needles or leaves, duff, grass, low shrubs
Ground Fuels
deep duff, roots, rotten buried logs, peat
Horizontal Continuity of Fuels
occurs when fuel source is continuous and has no patches, allows fire to spread easily as opposed to a patchy fuel source
Vertical Continuity of Fuels
allows the fire to climb vertically due to a continuous vertical fuel source
Moisture Content of Fuels
can deter the spread of fire temporarily
Chemical Content of Fuels
can limit or enhance spread of fire
Ignition
a temperature of 600 degrees F is required to ignite wildland fuels
Low Intensity Fire
weak indraft at fire’s edge, limited updraft and smoke column, environment controls the fire
High Intensity Fire
strong indrafts at fire’s edge, strong updraft and smoke column, fire controls the environment, alters weather elements
Factors Affecting Rate of Spread
wind speed, steepness of slope, changes in fuel type
Fire Weather Watch
means critical fire weather conditions are possible but not imminent or occurring
Red Flag Warning
issued when fire conditions are ongoing or expected to occur shortly
Amarillo Red Flag Criteria
minimum relative humidities equal to or less than 15%, 20ft winds of 20 mph or higher and/or gusts of 35 mph or higher, NFDRS adjective fire rating of High or higher
St Louis Red Flag Criteria
sustained 20ft winds >15mph, relative humidity <25%, 10 hr dead fuel moisture <9%
Extreme Fires
one or more criteria must be met: moving fast, prolific crowing and/or spotting, presence of fire whirls, strong convection column
Backfire
starting a fire separate from the wildfire to burn up potential fuels to prevent the fire from spreading further
Annual Average Acres Burned
has gone down since 1920 but has begun to rise since 2000
Prescribed Fires
acres burned and cost have gone up since 1995, as we have realized their importance
Change in Wildfire Patterns
megafires have become more frequent, more destructive, and more deadly, warmer climate causes drier conditions and longer wildfire season
Areas at Risk
western U.S. wildfires increasing in area, number of homes built in wildfire prone areas has increased
States most at Risk of Wildfires
California has the most houses in wildfire prone areas and had the most fires and acres burned in 2023 with Texas and North Carolina ranking highly as well
Evacuation Problem
too many houses in wildlands, traffic builds up on two lane roads
Smoke Effects
ash and particulate matter in smoke poses most risk to those in affected areas, painted surfaces, pipes, plastics, etc contribute to the dangerous smoke
Pyrocumulonimbus Clouds
fires produce updrafts, causing air to cool into clouds potentially causing thunderstorms, lightning can cause more fires
Tropical Cyclone Direction
counterclockwise in NH and clockwise in SH
Tropical Cyclone Ingredients
sea surface temp of at least 27C (80F)
warm, humid, unstable air
significant distance from the equator
weak wind shear
Tropical Cyclone Life Cycle
tropical disturbance → tropical depression → tropical storm → hurricane
Tropical Depression Criteria
cyclone with maximum 1-minute sustained surface winds of 33 knots (38 mph) or less
Tropical Storm Criteria
cyclone with maximum 1-minute sustained surface winds of 34-63 knots (39-71 mph)
Hurricane Criteria
sustained surface winds of 64 knots (74 mph) or greater
Tropical Cyclones
converging winds cause warm, moist air to rise rapidly, and rising air cools to the dew point temperature starting condensation (warming process), warmer air leads to stronger updrafts
Surface Air Pressure in Cyclone
highest air pressure at outer edge of cyclone, lowest in the eye
Wind Speed in Cyclone
highest in eye wall, lowest in eye
Eyewall
strong storms surrounding eye of the cyclone
Eyewall Replacement Cycle
outer rain band strengthen into band of thunderstorms, becoming the outer eyewall, replacing inner eyewall as it narrows
Saffir-Simpson Scale
classifies hurricanes into 5 categories based strictly on sustained wind speed, does not measure anything else
Tropical Cyclone Severity Scale (TCSS)
provides a category for each hazard (wind, surge, and rain), combined score for final category
States that Experience most Hurricanes
florida, texas, and louisiana
El Nino Effect on Hurricanes
less common when el nino is present, more frequent when its absent
North Atlantic Basin Season
June 1 to Nov 30
Eastern Pacific Basin Season
May 15 to Nov 30
Deadliest Hurricane to hit the US
1900 galveston storm, cat 4, 8,000 deaths, predates satellites
Tropical Cyclone Fatalities
outside of large events, number of deaths is decreasing
US Hurricane Deaths
1970-1999 inland floodings accounts for the most deaths, 1963-2012 storm surge accounts for most deaths
Storm Surge
abnormal rise of water generated by a storm, affected by maximum winds, speed of hurricane, size of storm, coastal features
Strongest Quadrant of Cyclone
front right quadrant of the storm, most tornadoes that form in TC form here as well
Flooding
determined by how fast the TC is moving, terrain, hydrology, land use
Forecast Cone
represents probable track of center of tropical cyclone, expected to remain within the cone 60-70% of the time
Hurricane Mitigation
reinforce buildings, covered windows, remove debris, emergency kit, have a plan
Ganges-Brahmaputra Delta Cyclone
east pakistan, most deadly tropical cyclone ever, estimated 400,000 dead, peak winds of 115 mph
Flood Fatalities
top three in deaths due to severe weather, most caused by flash floods, less caused by river floods, 52% caused by vehicles driven into water
US Flood Fatalities
highly variable year to year, not decreasing, younger than 20s and older than 60 more vulnerable
Flood Impacts on Human Health
transport debris and other contaminants, contaminate drinking water, leave mold, disrupt access to health care, injuries and deaths
State with Highest Flood Fatalities
texas, specifically in San Antonio and Houston
Cause of Kentucky Floods
areas of steep terrain development in low-lying areas, increase in rainfall events, deforested areas from past coal mining
Flash Flooding
local and sudden flood, lasts for short time after a few hours of rainfall, causes many deaths, thunderstorms far away can cause flash flooding in canyon areas
Regional Floods
huge, long lasting floods due to prolonged heavy rains over an extensive region