Study Guide Questions (All Subjects) Flashcards
- The steps in the hydrologic cycle
- How evaporation and condensation relate to saturation and the formation of clouds
Evaporation and condensation determine saturation (i.e. how much moisture is in the air)
We need air to rise to reach saturation. Clouds form when air rises, cools, and water condenses. Water vapor needs something to condense onto (microscopic particles). Clouds are composed of tiny liquid water droplets
- How changing temperature or water vapor changes RH
Higher temperatures and more water vapor in the air increase RH
- What dew point is and how it represents the amount of water vapor in the air
Dew point is the temperature at which saturation occurs. Dew point indicates the amount of water vapor vs RH which indicates how close to saturation. Higher dew point = more water vapor in the air
- Understand the 5 major “cloud terms” that make up the 10 main cloud types and the information they provide about where the cloud is, what the cloud looks
cirro = high, wispy
alto = mid level
cumulus = low base, grows tall
nimbo = indicates rain cloud
strato = low, sheet-like
- How winds blow around low-pressure and high-pressure systems (and what we call these systems), which are associated with rising/sinking air, and which are associated with good/bad weather.
Low-pressure system: Cyclones, Rising Air, Bad weather. Wind blows counter-clockwise and in
High-pressure system: Anticyclone, Sinking Air, Good weather. Wind blows clockwise and out
- What wind shear is
changes in wind speed and/or direction with height
- How are air masses classified? What are the 5 main air masses in North America, where
(generally) do they originate, and what kind of conditions do they bring?
Air masses are classified according to the moisture content and temperature of the surface underlying where they form
A = Arctic air mass found over the North Pole
P = Polar air masses found at high latitudes
T = Tropical air masses found near the equator
m = maritime air masses develop above oceans (wetter)
c = continental air masses form over continents (drier)
cT meaning of “Summer only in US” slide 29
only in summer
What are the 5 main air masses?
cA: Continental Arctic; forms over permanent snow or ice in the Arctic; extremely cold and dry
cP: Continental Polar; forms over northern North America, Europe, and Asia… Dry and cold
cT: Continental Tropical; forms over continental interiors; brings hot and dry summers as it moves east of north
mP: Maritime Polar; cool, moist air; forms over N. Atlantic, Pacific, and Southern oceans. Rain to west coast, snow to inland mountains
mT: Maritime Tropical; hot and humid summers; forms over tropical Atlanta, Pacific Ocean, and Gulf of Mexico then moves inland, affecting the SE states the most
*Thunderstorms and tornadoes: associated with weather patterns that form when mT meets cP
- The differences between the 3 NWS alerts (Atmosphere)
Advisory: potentially hazardous conditions
Watch: atmospheric conditions favoring hazardous weather over a region in time; actual location and time not known (e.g. ingredients are there)
Warning: imminent or occurring hazardous weather over a region in time
- What an omega block and ridge are, and how this leads to heat waves
Stationary anticyclone creates a broad ridge that pushes warmer air further north than usual; poleward extension of contour lines indicates warmer than normal. The ridge forms an omega block which prevents cooler air from penetrating the ridge and re-routing the cooler air around the ridge.
Stationary high pressure warm air leads to heat waves; increased solar radiation reaches the ground continuing to warm the surface and build pressure.
Extreme heat events in tropical or monsoon climates are caused by hot winds flowing in from nearby deserts related to sinking air and semi-permanent high-pressure systems near 30° north and south
Less moisture 🡪 clear skies 🡪 increasing solar radiation 🡪extreme heat
- What heat index and wet bulb temperature are, including threshold of survivability
Heat index: combines temperature and RH to think about risk to the human body
Wet bulb temp: the coolest you can make the air by evaporating water into it
Survivability threshold: wet bulb temperature greater than or equal to 35 degrees C; upper limit of safety beyond which the human body can no longer cool itself by evaporating sweat from the surface of the body to maintain a stable body core temp
- The 5 types of drought and the main causes of drought
Meteorological: prologues period of dry weather patterns
Hydrological: low water supply in lakes, reservoirs, rivers
Agricultural: damage to crops due to water shortage
Ecological: ecological damage from low soil moisture
Socioeconomic: demand for things like water, food grains, and fish increases due to a water shortage causes a deficit in supply
Drought causes
Less rainfall than normal due to high pressure systems
Warmer temps: increased evap leads to decrease in soil moisture
Surface and subsurface water removed
- What’s in the fire triangle, types of wildfires, and fuels of wildfires
Fire triangle: oxygen combines with carbon, organic plant material, and hydrogen
Types of fires
Ground fires: burn organic matter in the soil beneath surface litter and are sustained by glowing combustion
Surface fires: spread with a flaming front and burn leaf litter, fallen branches and other fuels located at ground level
Crown fires: burn through the top layer of foliage on a tree (canopy); most intense; requires to strong winds, steep slopes, and a heavy fuel load
Fire fuels
grasses: ignite easily; small-scale; strong winds escalate
shrubs (2-12 ft); loose layers allow for easy burning; plants with high content of natural oils are highly flammable
forests: if there isn’t much organic litter on the ground, the fire passes through with minimal damage to the tree; if there is a lot of organic litter on the ground, the fire burns hot and slow killing trees; shrubs act as ladders for crown fires
- The primary and secondary causes of wildfires in the U.S.
Primary: arson
Secondary: lightning
- The 4 factors that influence the spreading of wildfires
Different heights of trees: ladder fuels = fires can climb grasses to shrubs to trees
Santa Ana winds: strong wind burns a supply of fresh oxygen; spreading burning embers (firebrands) to start new blazes
Topography: fires burn faster up a slope
Invasive species: some non-native vegetation needs more water than available on average; invasive organisms can kill/damage trees
- How to mitigate fire threats to forests and property
Stop the fire triangle: add water, chemical retardants, and vegetation
Prescribing small fires to reduce wildfire intensity and decrease the likelihood of crown fires
Creating fire breaks
Create defensible space around homes:
Immediate: 0-5 ft
Intermediate: 5-30 ft
Extended: 30-100 ft
- How to get lows to strengthen
- The 4 types of fronts and what each looks like on a weather map. What are the features you see in a side view of a warm front and cold front (especially precipitation occurrence/types and temperature)? What is a dry line?
The 6 steps of polar front theory. In what stage of polar front theory is a mid-latitude low
strongest? Why?
- The difference between cyclogenesis and a bomb
- The different precipitation types (liquid, frozen, mixed) and how each forms
- The criteria for a storm to be a blizzard
- The differences between nor’easters, post-tropical cyclones, and subtropical cyclones
- What wind chill is
- How a wavy jet stream can cause cold outbreaks (polar vortex)
- What are the requirements for a thunderstorm to be considered severe?
- What features are found in a supercell thunderstorm (guest front, wall cloud, shelf cloud, roll cloud, mammatus cloud)? How does wind shear create the rotating updraft?
- Why and when thunderstorms develop along the dryline