Answer:
1. albedo - ability of a material to reflect solar radiation
2. conduction - transfer of heat between two stationary entities
3. convection - process of heat transfer by the circulation or movement of a liquid or a gas
4. Earth's energy budget - balance between the amount of energy coming in from the Sun and going back out into space
5. humidity - moisture in the air
6. latent heat - heat released when water vapor condenses
7. radiation - transfer of heat or energy through rays of various wavelengths
Explanation:
Heat comes in may different forms. In conduction, heat travels between two surfaces as a result of particle vibration. In radiation, heat travels through space. It travels as a result of the radiation waves of different wavelengths. The humidity measures the amount of moisture in the air. It is expressed as a percentage. In addition, the latent heat is "hidden heat" released when heat is released from water vapor at 100 degree Celsius,
D, folded should replace tilted :)
The three main types of mountains derive their names from how they form. Since it takes millions of years for mountains to form, there are some events that help mountains to form as they are. One is the collision of plates. The second is caused by the eruption of volcanoes. The third is the formation of mountains generated along mountain fault lines with some large blocks of rock forcing themselves upwards while others are forcing themselves down.
Answer:
ill explain on the bottom
Explanation:
Disadvantages of Choropleth Maps
Although choropleths give a good visual impression of change over space there are certain disadvantages to using them:
They give a false impression of abrupt change at the boundaries of shaded units.
Choropleths are often not suitable for showing total values. Proportional symbols overlays (included on the choropleth map above) are one solution to this problem.
It can be difficult to distinguish between different shades.
Variations within map units are hidden, and for this reason smaller units are better than large ones.
Isopleth maps
Isopleth maps differ from choropleth maps in that the data is not grouped to a pre-defined unit like a city district. These maps can take two forms:
Lines of equal value are drawn such that all values on one side are higher than the "isoline" value and all values on the other side are lower, or
Ranges of similar value are filled with similar colours or patterns.
This type of map is ideal for showing gradual change over space and avoids the abrupt changes which boundary lines produce on choropleth maps. Temperature, for example, is a phenomenon that should be mapped using isoplething, since temperature exists at every point (is continuous), yet does not change abruptly at any point (like population density may do as you cross into another census zone). Relief maps should always be in isopleth form for this reason.
Answer:
Kabihasnan sa lambak ng ilog. ... Ang isang ilog ay nagbibigay sa mga naninirahan ng isang maaasahang mapagkukunan ng tubig para sa pag-inom at agrikultura. Kabilang sa mga karagdagang benepisyo ang pangingisda, mayabong na lupa dahil sa taunang pagbaha, at kadalian ng transportasyon. Ang mga unang mahusay na sibilisasyon, tulad ng mga nasa Mesopotamia at Egypt, ang lahat ay lumaki sa mga lambak ng ilog.
Answer:
Erosion. the process of wearing away and movement of soil by fast moving water.
Depostion. the process of soil being dropped off by slow moving water.
head. the beginning of a stream or river where runoff begins to cut a channel.
Mouth. ...
Delta. ...
Floodplain. ...
trunk. ...
tributary.
Explanation:
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