Section 1

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Planck function

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Last updated

6 years ago

Date created

Mar 1, 2020

Cards (57)

Section 1

(50 cards)

Planck function

Front

- A distribution of wavelengths of emitted radiation, which has a characteristic slope. Wavelength by Energy density.

Back

water transfer

Front

- driver of ocean circulation, evaporation, precipitation

Back

Angular momentum conservation

Front

- if a rotating object moves closer to its axis of rotation, it must speed up to conserve angular momentum

Back

Halocline

Front

- salinity increases rapidly around 100m depth

Back

Blackbodies

Front

- Objects that emit with 100% efficiency (radiation)

Back

Solar radiation

Front

- Radiation emitted by sun, almost all liught in earths atmosphere with a wavelength less than 3 microns

Back

Sensible Heat Flux

Front

- fast moving molecules of substance 1 collide with neighboring molecules of substance 2, which are moving more slowly. This forces the molecules of substance 2 to speed up. Substance 2 becomes hotter as a result of its physical contact with substance 1. This form of heat transfer often occurs between the atmosphere and the earth's surface. Positive is flux from surface to atmosphere.

Back

Temperature

Front

- ocean heated from above, warmest temperatures near the surface of the ocean

Back

oceanic uptake

Front

- one main way anthropogenic CO2 is removed from the atmosphere, bc elevated atmospheric CO2 concentrations a bit more dissolves in seawater than normal, this extra carbon is transformed to toeher molecules and ions containing carbon, these taken up by marine organisms, part of carbon incorporated into the skelton of marine organisms and buried in deep sea sediments as organisms die and fall to the bottom of the ocean

Back

Density

Front

- function of temperature and salinity, warmer water is less dense, saltier water is more dense, warmer + fresher = less dense so very stable environment with little vertical motion, especially below 100m

Back

Terrestrial Radiation

Front

- Radiation emitted by the earth, almost all light in earth's atmosphere with a wavelength greater than 3 microns comes from the earth or the atmosphere

Back

Chlorophyll

Front

- makes plants green, chemical responsible for photodynthesis, can see phytoplankton in ocean;s main upwelling zones, because dead biological materials tend to sink, so deep waters rich in nutrients

Back

Latent Heat Flux

Front

- A liquid evaporates into an overlying gas, a process which requires energy and therefore removes heat from the liquid. This also occurs between the atmosphere and earth's surface. Directly proportional to evaporation (used interchangeably).

Back

Thermohaline circulation

Front

- overturning circulation, density of surface water in atlantic greater than other oceans due to high salinity, in northern winter, atmosphere extreacts huge amounts of heat from waters of north atlantic, water can become dense enough to sink to the bottom of the ocean, initiates the oceans' deep overturning circulation, after sinking this water slowly spreads throughout the global ocean and eventurally returns to the surface, thermos refers to fact driven by cooling of N atlantic surface waters, haline refers to face it is drien by waters high salinity

Back

Cenozoic era

Front

- the rise of mammals, divided into epochs (more fine grained division as we approach present)

Back

Equatorial upwelling

Front

- driven by Ekman drift, near equator, trade winds blow toward the west, Coriolis force acts in opposite directions in two hemispheres, so cold deeper water forced to surface

Back

sea ice

Front

- much more reflective of sunshine than seawater (has higher albedo), thus the presence of seas ice has a profound influence on how much of the sun's heat energy the earth absorbs, closely linked to temperature and exhibits a pronounced seasonal cycle in both hemispheres, covers largest area in late winter and smallest in summer

Back

Greenhouse Gas

Front

- a gas that absorbs significantly the terrestrial radiation emitted by the earth and its atmosphere

Back

Precipitable water

Front

- total amount of water vapor in the atmospheric column

Back

Hadley cell

Front

- atmospheric circulation cell, air is warmed and rises near equator, creates cloudiness and precipitation, diverges aloft and makes way to subtropics, sinks in subtropics and flows back to equation

Back

CO2 fertilization

Front

- causes terrestrial biosphere to absorb anthropogenic carbon, plants obtain CO2 for photosynthesis through stomata, also lose water through stomata so need to control size, when CO2 concentration increases stomata do not need to be as large, so plants can survive under drier conditions

Back

Clausius-Clapeyron relation

Front

- the relationship between the mixing ratio of water vapor at saturation and temperature

Back

Coriolis force

Front

- all objects moving in the northern hemisphere are deflected to the right, and southern hemisphere to the left, curved trajectories of objects moving on the earth's surface

Back

Relative humidity

Front

- ratio of the amount of water vapor in the air to the amount of water vapor that the air would hold if it were saturated

Back

Intertropical Convergence Zone

Front

- band of cloudiness associated with the rising branch of the Hadley cell in the deep tropics

Back

Climate

Front

- the statistics of weather, "what you expect"

Back

climatologies

Front

- long-term averages (Seasonal variation of surface air temperature, precipitable water, rising motion, and precipitation)

Back

Inverse-Square Law

Front

- The total flux of radiation transferred from one object to another varies according to the distance between the two objects, the total flux of energy transferred from one object to another aries according to the distance between two objects

Back

Environmental Justice

Front

- the fair treatment and meaningful involvement of all people regardless of race, color, national origin, or income with respect to the development, implementation, and enforcement of environmental laws, regulations, and policies.

Back

Cretaceous period

Front

- roughly 144-65 million years ago, dinosaurs were the dominant large animals and the climate was hot, CO2 levels were at least 4 times higher than currently, no ice, sea level higher, deep ocean temperatures warmer, major biomes were shifted 15 degrees poleward of present

Back

Pleistocene epoch

Front

- last 2 million years, produced ice ages

Back

Mesozoic era

Front

- subdivision of Cambrian era, when the dinosaurs roamed, ended with a bang 65 million years ago

Back

Anthropocene

Front

- a new geologic era, the current geological age, viewed as the period during which human activity is the dominant influence on climate and the environment.

Back

Greenhouse Effect

Front

- Terrestrial radiation is both absorbed and emitted in the atmosphere... MORE!

Back

Ekman drift

Front

- the mechanical response o the ocean to wind blowing across its surface, surface water dragged along with thte wind, due to Coriolis force it is deflected somewhat to the right in the northern hemisphere, surface water drags along the water immediately beneath it but at a slower speed, this layer deflected to the right uner the influence of the coriolic force, result is a spiraling pattern in the current direction w/ ever decreasing current speeds with depth, net transport of water is to the right of the wind 90 degrees, and v.v

Back

weather

Front

- evolution of atmosphere on short time scale (days to months)

Back

Mid-latitude jet stream

Front

- a strong eastward storm track(?) in both hemispheres at about 45-60 degrees due to Hadley cells

Back

Area under curve of Planck function

Front

- Total energy emitted by the object, proportional to the fourth power of the objects temperature. > known as Stefan-Boltzmann Law = the energy emitted increases very quickly as the objects temperature increases.

Back

Cambrian explosion

Front

- the sudden explosion of biodiversity and complexity, approx.. 580-545 million years ago much more complex life forms emerged including nearly all categories of animals Pre-cambrian era and Cambrian era - before and after

Back

Salinity

Front

- measured in parts per thousand, because of influence of precipitation, freshest waters located nearest the surface

Back

Peak Wavelength

Front

- Of Planck function, inversely proportional to the temperature of the object, the hotter the object the shorter the typical emission wavelengths

Back

Net Solar Radiation

Front

- at top of earth's atmosphere = incoming - reflected

Back

Albedo

Front

reflectivity of the Earth

Back

momentum transfer

Front

- important for surface circulation, takes place through frictional effects of winds on the ocean surface

Back

Electromagnetic Spectrum

Front

- radiation organized according to their wavelengths (small > large)

Back

reforestation

Front

- one process that causes the terrestrial biosphere to absorb anthropogenic carbon

Back

Heat transfer

Front

- driver of ocean circulation across air-sea interface, latent heat flux, sensible heat flux, radiation

Back

upwelling

Front

- feature of surface ocean circulation, upwelling is the upward movement of water towards the surface, because of vertical temperature structure of the ocean, this water is almost always cold relative to the water it replaces

Back

Peer-review process

Front

- Other scientists evaluate and criticize work, leading to reisions and resubmission of improecd manuscript

Back

Thermocline

Front

- temp drops off very quickly around 100m

Back

Section 2

(7 cards)

ice ages

Front

- cold state, climate of last glacial maximum

Back

orbital forcing

Front

- the notion that variations in earths orbit might be connected to the variations in earths past climate was pioneered over 100 years ago by Milutin Milankovitch

Back

solstices

Front

- occur on dec 21 and june 21, times in calendar year when the earths spin axis is tilted perfectly toward or awary from the sun, moments when one of the hemispheres receives its maximum sunchine, and the other its minimum

Back

feedback process

Front

- the climate warms and greenhouse gases increase, greenhouse gas increase causes climate to warm further which leads to more greenhouse gas increase and so on, this also has powerful implications for the future role of the carbon cycle

Back

interglacial periods

Front

- warm state, the climate that characterized recorded history

Back

equinoxes

Front

- march 21, sept 21, the times when the earths spin axis is pointed neither toward nor away from the sun, both hemispheres receive same amount of sunshine

Back

Sturtian

Front

- our cold period occurred in the late pre-cambrian, roughly 720-660 million years ago, snowball earth

Back