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Cloud [144]
3 years ago
8

Jet streams are fast-moving streams of air high above Earth's surface. A divergence or convergence in the jet stream above a hig

h- or low-pressure center can drive the actions of these pressure centers. If the air in the jet stream is converging or diverging faster than the air at the surface is moving out or in, the driving force of the jet stream is compensated by an increase in surface winds.
A jet stream generally diverges above a low-pressure (warm) center. However, at Earth's surface, air converges at a low-pressure center. If the divergence of the jet stream is greater than the convergence of air at the surface low-pressure center below it, what will happen to the surface winds?
Geography
1 answer:
notsponge [240]3 years ago
6 0

Answer:

The surface wind will most likely get stronger.

Explanation:

The magnitude of surface wind is dependent on several factors such as the pressure gradient, centrifugal acceleration, primary and secondary winds. The movement of jet streams above the surface of the Earth influences the factors that affect the magnitude of the surface wind. An increase in the jet stream driving forces makes the surface wind more stronger.

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The decay of radioactive elements such as uranium creates ______, especially in Earth's crust, where these elements are abundant
Natalija [7]

Based on the knowledge about radioactive elements, the decay of radioactive elements such as uranium creates heat especially in Earth's crust, where these elements are abundant.

<h3>What are radioactive elements?</h3>

Radioactive elements are elements which undergo spontaneous decay of their nucleus and in the process produce elements with smaller atomic masses with the release of radiation and heat.

Examples of radioactive elements include uranium and radium.

Therefore, the decay of radioactive elements such as uranium creates heat especially in Earth's crust, where these elements are abundant.

Learn more about radioactive elements at: brainly.com/question/18640165

7 0
2 years ago
How do scientists determine the relative age of rocks?
NISA [10]

Answer:

Super position

Faunal Succession

Crosscutting Relationships

Inclusions

Explanation:

Superposition: The most basic concept used in relative dating is the law of superposition. Simply stated, each bed in a sequence of sedimentary rocks (or layered volcanic rocks) is younger than the bed below it and older than the bed above it. This law follows two basic assumptions: (1) the beds were originally deposited near horizontal, and (2) the beds were not overturned after their deposition.

Faunal Succession: Similar to the law of superposition is the law of faunal succession, which states that groups of fossil animals and plants occur throughout the geologic record in a distinct and identifiable order. Following this law, sedimentary rocks can be “dated” by their characteristic fossil content. Particularly useful are index fossils, geographically widespread fossils that evolved rapidly through time.

Crosscutting Relationships: Relative ages of rocks and events may also be determined using the law of crosscutting relationships, which states that geologic features such as igneous intrusions or faults are younger than the units they cut across.

Inclusions: Inclusions, which are fragments of older rock within a younger igneous rock or coarse-grained sedimentary rock, also facilitate relative dating. Inclusions are useful at contacts with igneous rock bodies where magma moving upward through the crust has dislodged and engulfed pieces of the older surrounding rock.

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