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weather
day-to-day variation in the atmosphere
climate
the statistical description of weather over some period of time (usually a few decades)
climate scientists tend to focus on:
temperature and precipitation
precipitation
all liquid or solid phase aqueous particles that originate in the atmosphere and fall to earths surface
name the 5 climate systems
atmosphere
hydrosphere
biosphere
lithosphere
cryosphere
atmosphere
the thin layer of gases that surround the planet
what are the three main gases in the atmosphere
nitrogen, oxygen, argon
what percentage of the air is nitrogen
78%
what percentage of the air is oxygen
21%
what percentage of the air is argon
1%
what is a variable gas
type of gas in the atmosphere whose concentration can change over time and space
what are the variable gases
water vapor
carbon dioxide
ozone
methane
nitrous oxide
the most variable gases are the _________ gases
greenhouse
Greenhouse gases are great at ________ heat
absorbing
temp profile:
change in temp with height, usually displayed as temp on the X-axis and height on the Y-axis
Lapse Rate:
how quickly temp changes with height. (C/km
temp inversion:
a negative lapse rate; temp increasing with height
what are the main layers of the atmosphere
troposphere
stratosphere
mesosphere
thermosphere
what layer of the atmosphere does most weather occur
troposphere
what layer of the atmosphere is the boundary layer
troposphere
in the troposphere, temp _________ with height
DECREASES
tropopause:
the boundary layer between the troposphere and the stratosphere. (boundary for thunderstorms)
in the stratosphere, temp ___________ with height
INCREASES
what is it called when temp INCREASES with height
an inversion
which layer of the atmosphere contains the ozone layer
stratosphere
inversion exists in the stratosphere because of the
ozone layer
in the mesosphere, temp ________ with height
DECREASES
in the thermosphere, temp __________ with height
INCREASES
temp: the _________ of gas molecules
kinetic energy
density: __________ of gas molecules in a defined ____
amount/mass, volume
pressure: _______ of gas molecules
weight/force
pressure _______ exponentially with height
decreases
__________ movement of air can result in convergence or divergence
horizontal
convergence:
winds come together; colliding
divergence:
winds separating
areas of convergence are areas of _______ air
rising
areas of divergence are areas of ________ air
sinking
_______ air is needed to form clouds and precipitation
RISING
convergence associated with areas of ____ pressure at the surface
LOW
counterclockwise spin
areas of low pressure
counterclockwise spin→ low pressure→
converge
divergence is associated with areas of _____ pressure
HIGH
clockwise spin
areas of high pressure
clockwise→ high pressure→
diverge
wind blowing at 0 degrees, what direction is that?
north
winds blowing at 90 degrees, what direction is that?
east
wind is blowing at 180 degrees, what direction is that?
south
wind is blowing at 270 degrees, what direction is that?
west
Energy surplus at the equator and a deficit at the poles.
surplus= temp _______
deficit= temp ________
increase, decrease
the net imbalance btw the equator and poles drives ______ and ______________.
atmospheric and oceanic circulations
the sun drives atmospheric circulations, referred to as the ________________
general circulation model
what is the goal of the atmospheric and oceanic circulations?
to achieve balance (redistribute the heat from the equator
thermally direct:
transport heat from warmer regions to cooler regions
thermally indirect:
transport heat downward and equator-ward
what force causes the circulation model to have 3 cells on each hemisphere instead of 1 big cell
the Coriolis force
the Hadley cell circulated air btw the ______ and __________
tropics and subtropics
Intertropical convergent zone: zone of low pressure (rising air) at/near the equator
this region is characterized by heavy rain falls and relatively light winds (Koppen A)
its position varies seasonally: closer to 10 degrees in july and south of the equator in january
Rising Branch of the Hadley cell at the Equator: ITCZ
Intertropical convergent zone: zone of ____ pressure (rising air) at/ near the equator
low
as the air moves north from the equator; two things happen
the flow moves to the RIGHT
the flow ACCELERATES
This branch includes the subtropical jet stream
The pole-ward upper air branch of the Hadley cell
subtropical jet stream:
a fast, eastward, moving ribbon of air located around 30° latitude in both hemispheres
air traveling pole-ward merges w/ thee subtropical jet
this merger creates convergence in the upper atmosphere
this means there must be sinking air and diverges at the surface
subtropical high
all of this sinking air at 20-30 degrees latitude creates high pressure at the surface, the sinking air warms adiabatically
all of this combines to produce warm, dry conditions (most of the world’s deserts are found at this latitude)
Descending branch at 30 degrees latitude
remember, air travels away from HIGH pressure in a CLOCKWISE motion, so some air is sent back to the equator
once again, we have factor Coriolis
The result is a belt of Northeasterly winds called trade winds.
Equator-ward branch at the surface
the convergence of the NE Trade winds in the N. Hemisphere and the SE Trade winds in the S. Hemisphere contribute to the __________ at the ITCZ
convergence
the Ferrel cell circulates air btw the __________ and the __________
subtropical highs and the subpolar lows
which of the 3 cells are responsible for most of our weather?
ferrel cell
in the Ferrel cell, air traveling north from the subtropical high is deflected to the right by Coriolis. the result is a belt of
westerly winds across the mid-latitudes bringing warm air pole-ward.
which cell is not based on temp differences and is purely mechanical → indirect circulation
ferrel cell
the polar cell, circulates air between the cold ___________ and the ____________
polar high pressure, subpolar low pressure
in the polar cell, air diverging from high pressure travels south, Coriolis deflects it to the right, the result is
polar easterlies: bringing polar air south
the cold polar easterlies meet the warm(ish) midlatitude westerlies around 60 degrees latitude. this zone is know as the
polar front
the strong temp gradient between the two air masses (polar easterlies and midlatitude westerlies, i.e the polar front) creates another important feature in this region called the
polar jet
the subtropical jet is formed by mainly earths rotation and the temperature contrast between the tropical and subtropical regions. but the polar jet is formed by
the temperature gradient between the polar and mid-latitudes regions, closely related to the polar front
in the winter the polar jet is found further south (responsible for cold air outbreaks) and the jet winds are faster bc of
greater temp contrast
true or false, subtropical jet and polar jet flow directly west-to-east
false, they do flow west-to-east but are organized in patterns of troughs and ridges
due to the trough and ridge patterns of the subtropical and polar jet, cold air moves
equator-ward
due to the trough and ridge patterns of the subtropical and polar jet, warm air moves
pole-ward
the trough and ridges of the polar jet stream that move cold air equator-ward and warm air pole-ward to try to fix the energy imbalance, the N. hemisphere is encircles by several of these waves and they are called
Rossby or longwaves
Rossby waves have 3 distinct flow patterns which are:
zonal, meridional, and split flow
zonal flow:
small amplitude waves result in a west-to-east flow pattern. the flow is nearly parallel to the lines of latitude. cold air tends to remain pole-ward
meridional flow:
highly amplified troughs and ridges. in this patten, cold air flows toward the equator and warm air floes pole-ward
Split flow:
occurs when you have zonal flow near the poles and meridional patterns further south.
variation in temp indicates an ______ in energy
imbalance
if energy received is greater than energy released, temp ________
increases
if energy received is less than energy released, temp _______
decreases
Which heats and cools quicker: barren land or water
barren land
barren land will heat and cool quicker than water, why?
specific heat!
specific heat:
the amount of energy needed to increase the temperature of 1 g of a substance by 1 degree C
Aspect:
the direction that a mountain slope faces
south facing aspect will be
warmer, drier and have less vegetation in the N. Hemisphere
clouds _____ solar energy above the cloud and _____ warming below the cloud during the day
reflect, reduce
seasonality in the midlatitudes defined more by ________
temperature
seasonality in the tropics more sharply defined by _______
precipitation
teleconnection:
a linkage between weather changes occurring in widely separated regions of the globe
ex: ENSO, NAO, PDO, AMO, MJO, AO
what does ENSO stand for?
El Nino- Southern Oscillation
El Nino:
an ocean / atmosphere connection marked by the warming of the ocean off the western coast of South America. resulting in warmer than avg global temperatures.
La Nina:
an ocean / atmosphere connection marked by the strong cooling of the ocean off the western cost of South America. resulting in cooler than avg global temperatures.
what does ONI stand for?
Oceanic Nino Index
El Nino conditions officially present when
The ONI has been more than 0.5 C for more than 5 consecutive months
La Nina conditions officially present when
The ONI has been less than 0.5 C for 5 consecutive months
what does NAO stand for?
North Atlantic Oscillation