Part 2 Flashcards

1
Q

What is thermohaline circulation?

A

Movement of ocean water caused by density difference brought about by variations in temp (thermo) and salinity (haline). As ocean water freezes at the poles it concentrates salt, and the colder, denser water sinks.

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2
Q

What is the main driver of thermal circulation?

A

Deep water currents, difference in the waters density.

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3
Q

What is the tropical cyclone heat transfer mechanism?

A

Heat transfer occurs mainly in the form of latent heat, strongly influenced by sea surface ocean temperature, high level winds, wind shear, and coriolis force.

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4
Q

what is latent heat?

A

latent heat of melting and vaporization: the energy needed to accomplish phase transition or the heat required to convert a solid into a liquid or vapor, or liquid into vapor, without a change in temperature.

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5
Q

what causes monsoons?

A

-Seasonal reversing wind
-Draw tropical energy to higher latitudes
-Affect global atmospheric circulation

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6
Q

what are the characteristics of the North Atlantic Oscillation (NAO), Positives and Negative:

A

-Affects flow of energy across polar front
-Has impacts across Northern Hemisphere
-Changes positions of the polar jet stream

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7
Q

El Nino Southern Oscillation:
what is it?
what happens in the pacific region?
impact on the US?

A

-Anomalous climatic events, occur every 3-7 years
-coupled interaction between ocean and atmosphere in the tropical pacific
-collapse of southeast trade winds
-surface warm pool in western pacific move eastward
-upwelling shuts down off west coast of south America
-Unusually dry periods in some regions
-Higher than normal rainfall in other regions

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8
Q

what is the Pacific Decadal Oscillation and its features?

A

PDO: Pacific Decadal Oscillation
-Affects global temperature
-Global warming cannot predict PDO
-Similarities to ENSO, but much longer time scale (20-30years)

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9
Q

what is the Atlantic Multidecadal Oscillation and its features?

A

-Sea surface temp. anomaly oscillation in the north Atlantic
-estimated period of 60-80yrs
-possible connection to strength of the thermohaline circulation
-somewhat controversial, also the potential link to hurricane frequency

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10
Q

what are tropical cyclones?

A

Low-pressure systems that push water up. form over large bodies of relatively warm water. They derive thier energy through the evaporation of water form the oceans surface, which ultimately condenses into clouds and rain when moist air rises and cools to saturation

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11
Q

what are NADW and AABW

A

-North Atlantic Deep Water
-Antarctic Bottom Water

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12
Q

what are isotopes?

A

atoms of the same element with different number of neutrons

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13
Q

what is radiative forcing?

A

an imbalance between earths incoming and outgoing radiation

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14
Q

what is global dimming?

A

global dimming is the reduction in the amount of global direct irradiance at the earths surface that has been observed since the systematic measurements began in the 1950s

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15
Q

resulting heat uptake of ocean vs atmosphere?

A

oceans have absorbed 90% of excess energy. ocean circulation is not global/confined to one hemisphere.

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16
Q

what is meridional heat transport?

A

heat transport across latitudes prevents tropics from heating up and poles from cooling down.

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17
Q

what makes greenhouse gases different from the main constituents of the atmosphere?

A

-electric dipole moment is critical for interaction with electromagnetic radiation
-different absorption spectra for different gases

18
Q

what causes radiative forcing?

A

the change in concentration of carbon dioxide or the output of the sun

19
Q

what is the difference between climate sensitivity and radiative forcing?

A

a measure of how much earths surface will cool or warm after a specified factor causes a change in its climate system

20
Q

greenhouse effect:

A

some greenhouse gases allows for less heat to be trapped in the atmosphere and causes more heat to escape into space

21
Q

what does the observed stratospheric cooling indicate?

A

ozone is being depleted and an increase of CO2 in the troposphere

22
Q

Approximate Total Anthropogenic Forcing:

A

-48% abosrbed into the surface
-29% is reflected
-23% is absorbed into the atomosphere

23
Q

enhanced greenhouse effect:

A

more greenhouse gases allows for more heat to be trapped in the atmosphere and causes less heat to escape into space

24
Q

what is the evidence for anthropogenic activities being the main source of atmospheric CO2 increase?

A

economic data, carbon isotype data, and change in oxygen-to-nitrogen ratio in atmosphere.

25
Q

what can be derived from atmospheric carbon isotope studies in this context?

A

-plants and algae are depleted in d13c
-atmospheric CO2 is also depleted in d123c

26
Q

carbon reservoirs in the earths system and relative sizes:

A

-ocean is the biggest carbon pool
-land is the second biggest carbon pool
-atmosphere is the smallest carbon pool

27
Q

sources of anthropogenic carbon:

A

-fossil carbon
-land use charge
-ocean sink
-land sink
-atmosphere

28
Q

latitudes with dry and wet conditions:

A

-descending limbs of hadley cells are the sites of the worlds major desserts
-descending air warms adiabatrically and thus is dry because warm air can hold more moisture.

29
Q

coriolos effect, and impact on flowing air and water

A

-deflection of air or water by earths rotation, deflection in the Northern hemisphere to the right, deflection in the southern hemisphere to the left

30
Q

what are jet streams and ITCZ

A

polar jet streams dominate mid-latitude weather: fast upper level winds form at the boundary between cold and dense polar air and warm moist subtropical air

ITCZ is the inter tropical convergence zone

31
Q

what are examples of rapid fluxes in the earths system?

A

photosynthesis and respiration

32
Q

unequal heating of the earths surface, resulting in temperature gradient, energy imbalance between low and high latitudes:

A

CO2 dissolve in water and reacts to form carbon acid

CO2 addition to seawater lowers pH value

33
Q

how do phase transitions of water within the hydrological cycle contribute to energy transfer in the climate system?

A

the process of melting, evaporation and sublimation absorb energy. this added energy causes the molecules to change their bonding pattern. in the earth system, this energy must be supplied by the surrounding environment. thus, these phase changes result in cooling of the surrounding environment.

34
Q

what is special about what specific heat?

A

water has a high specific heat, meaning it takes more energy to increase the temperature if water compared to other substances.

35
Q

surface ocean circulation?

A

ocean surface currents are strongly affected by surface winds, the earths rotation, and the position of the continents.

36
Q

Gyres

A

Five major rotating systems:
North Atlantic Gyre, the South Atlantic Gyre, the North Pacific Gyre, the South Pacific Gyre, and the Indian Ocean Gyre—that have a significant impact on the ocean. The big five help drive the so-called oceanic conveyor belt that helps circulate ocean waters around the globe.

they form in large ocean basins, and they transfer and release heat energy. three forces cause circulation of gyres winds: global winds patterns, earth rotation and earths land masses

37
Q

warm currents vs cold currents

A

warm ocean currents originate near the equator and move toward the poles or higher latitudes while cold currents originate near the poles or high latitudes and move toward the tropics or lower latitudes.

38
Q

tropical divergence

A

the upper layers of the ocean diverging at the equator and drawing cooler, nutrient rich water towards the surface because of the impact of the surface winds.

39
Q

characteristics of the gulf stream

A

a powerful, warm, swift Atlantic ocean current that originated at the tip of Florida and follows the eastern coastlines of the united states. It is largely driven by wind stress

40
Q

characteristics of the circumpolar current

A

-eastward flow around antartica
-strongest ocean current (more than 100 sv)
-winds create a divergence at the surface
-deep water is mixed to the surface

41
Q

temperature and salinity distribution in surface ocean waters:

A

at mid-latitudes, salinity influences the depth to which water masses sink and how far they extend through the ocean