Answer:
1) 70
2) conduction
3) The ground absorbs the solar radiation and
releases it throughout the later afternoon.
4) transpiration
5) convection
6) cumulonimbus
7) reflectivity of Earth’s surface
8) As temperature increases, air pressure
increases.
9) thermosphere
10) convection cells, pressure belts, and the
Coriolis effect
11) radiation
12) pollen
13) scattering
14) thermosphere
15) The different types of clouds are:
<u>cumulus:</u><em><u> </u></em><em>Cumulus clouds are clouds which have flat bases and are often described as "puffy", "cotton-like" or "fluffy" in appearance. Their name derives from the Latin cumulo-, meaning heap or pile. </em>
<u>cirrus</u><em>:</em><em> </em><em>Cirrus is a genus of atmospheric cloud generally characterized by thin, wispy strands, that typically appear white or light grey. The name is derived from the Latin word cirrus, meaning 'ringlet' or 'curling lock of hair'. Such a cloud can form at any altitude between 5,000 and 13,700 m above sea level.</em>
<u>stratus:</u><em> </em><em>Stratus clouds are low-level clouds characterized by horizontal layering with a uniform base, as opposed to convective or cumuliform clouds that are formed by rising thermals.</em>
<u>nimbus</u>: <em>Nimbostratus clouds are dark, grey, featureless layers of cloud, thick enough to block out the Sun and produce persistent rain. Height of base: 2,000 - 10,000 ft. Shape: Bands or areas of individual cells. Latin: nimbus - rainy cloud; stratus - flattened or spread out. Precipitation: Continuous rain or snow likely.</em>
16) the tradewinds
17) the location’s latitude
18) Cirrus clouds
19) the ozone layer
20) Global winds are created by both the spin of
the Earth (Coriolis effect) and the differences
in temperature between the equator and
the polar areas. These winds are often
grouped together as trade winds, easterlies,
and westerlies.
21) nitrogen
22) the Miller-Urey hypothesis
the Oparin-Haldane hypothesis
23) ammonia gas
24) cumulus
25) It determines the mass of water in a volume of air
Explanation:
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