221 study this and cheat sheet Flashcards
surface station
- a weather observing location that reports weather conditions
- show temperature, pressure, wind, radiation, turbidity
IPCC SROC
- special report on the ocean and cryosphere in a changing climate
- 2019
- Observed changes and impacts, projected changes and risks, and implementing responses to ocean and cryosphere change
temperature
- the sensible heat at a given location
marine observations
- provide current information on the Ocean water
- info on sea surface temperature, surface winds, marine weather
moisture
- the precipitation and humidity
- the precipitation is water, in liquid or solid form, that falls from the atmosphere and reaches the earth
- humidity is the amount of water vapor in an air mass at a given time
pressure
- the weight exerted by an air mass
solar energy
- energy from the sun that is transformed into heat at or near the earth’s surface
radiation
- Can be absorbed or emitted by all matter, depending on temperature and “emissivity” of the material
- All objects warmer than 0 Kelvin emit radiation
Insolation
- The amount of incoming solar radiation
- not equal everywhere on Earth
- Amount depends on the intensity and duration of radiation from the sun
- these depend on the number of daylight hours and angle of the sun’s ray
three ways that precipitation can occur
- orographical- warm moist air rises over hills
- convectional- rising moist air that cools down
- cyclonic- cool and warm air masses meet
jet streams
- flow from west to east
- guide movement of weather systems
shortwave vs longwave radiation
- Shortwave radiation refers to high-energy radiation with shorter wavelengths (sun)
- Longwave radiation refers to lower-energy radiation with longer wavelengths (Earth)
- only shortwave is visable
high emission scenario vs low emission scenario
- high emission scenarios project continued, rapid increase in greenhouse gas emissions
- Ex: RCP8.5
- low emission scenarios look at substantial and substained reduction in greenhouse gas emission
- RCP2.6
why are Temperatures heavily moderated by large bodies of water?
- Some earth surface materials (like water) store solar energy more effectively than others
is cold or warm water more dense?
- cold water
energy balance
- the equilibrium between the amount of solar energy that Earth receives from the sun (incoming radiation) and the amount of energy it radiates back into space (outgoing radiation)
outgoing longwave radiation
- the heat that Earth radiates back into space
- differences in surface temperature makes OLR different across world
- determined by cloud amount and height, and surface temperature
heat transfer
- Heat transfers in air and ocean, which balances the surplus of energy in the tropics and the deficit of energy at the poles
greenhouse effect
- Natural process
- Certain gases in the Earth’s atmosphere trap heat from the sun, warming the planet’s surface
keeling curve
- A graph that shows us the concentration of carbon dioxide in parts per million
- Observed in Mauna Loa, Hawaii, where the Earth’s air is sampled
- concentration rises throughout the year, but then decreased in September
- This is because in the fall, plants decay and decompose, releasing CO2
- the entire curve has been increasing exponentially
albedo
- how reflective a surface is
- Earth’s albedo is reflected by clouds, aerosols, and the surface
- Ex: snow and ice have a high albedo and water has a lower one, absorbs more of the sun’s energy
- High allbedo surfaces bounce sunlight back
- about .30 for Earth as a whole
what temperature water holds more gas?
- cold water
ocean acidification
- A decrease in ocean pH over decades or more that is caused primarily by uptake of CO2 from the atmosphere (CO2 reacts with seawater to form carbonic acid)
- Because human activities are releasing CO2 into the atmosphere very quickly, the ocean is taking up CO2 faster today than it has in the past
plate tectonic theory
- Theory that Earth is composed of numerous plates that
move independently of one another at varying speeds, over the earth’s surface
ice albedo positive feedback
- Cooling produces more ice and snow cover, which further cools the Earth
- Warming reduces the ice and snow cover, which further enhances the warming
last glacial maximum
- A period in Earth’s climate history when ice sheets were at their maximum extension, between about 26,500 and 18,000 years ago
- Vast ice sheets covered much of North
America, northern Europe and Asia
holocene
- A period from about 11,500 years ago to present, characterized by relatively stable warm climate
6 land biomes
- Rainforests, deserts, grasslands, deciduous forests, boreal forests, tundra
2 water biomes
- marine (saltwater) and freshwater
phytoplankton
- absorb CO2 through the atmosphere through photosynthesis
- when they die, the CO2 sinks to the ocean floor and reenters the atmosphere
- this is called the biological pump
zooplankton
- eat phytoplankton and add more carbon to the ocean
- make the ocean a carbon sink
sunspot activity
- more sunspots deliver more energy to the atmosphere, so that global temperatures should rise
- A spot or patch appearing from time to time on the sun’s surface
- Can fluctuate year to year, and change all the time
Global Dimming
- A gradual decrease in the amount of sunlight reaching the Earth’s surface
- Anthropogenic aerosols are major cause for this anomaly
global brightening
- As air pollution has decreased in many areas, more sunlight is now reaching the planet, causing a “brightening” effect
- considered better than global dimming because brighening is associated with a reduction is atmospheric aerosols
kelvin boiling of water, freezing of water , and absolute 0
- boiling: 373.15
- freezing: 273.15
- absolute 0:0
Celcius boiling of water, freezing of water , and absolute 0
- boiling: 100
- freezing: 0
- absolute 0: -273
Fahrenheit boiling of water, freezing of water , and absolute 0
- boiling: 212
- freezing: 32
- absolute 0: -460
CO2 emission by source and from fossil fuel
- from source: land use and coal
- from fossil fuel: electricity generation and heating