As the spacing between isobars increases, the horizontal pressure gradient force and wind speed decrease.
The closer the spacing of isobars, the stronger is the strain gra- dient force. The stronger the stress gradient pressure, the stronger is the wind. thus, intently spaced isobars mean strong winds; extensively spaced isobars imply lighter wind.
The relationship between isobar spacing and wind velocity is that the closer the isobar spacing then the stronger the wind velocity. The spacing among isobars represents a stress differential among those two isobars. when two isobars are nearer together then the stress changes at a greater rate over distance.
The lines around high and low strain on a climate map are called isobars, or lines of equal stress, as shown in the above image on the left. While isobars are near together it is very windy; while they are further aside, conditions are more calm. The wind around highs usually blows in a clockwise direction.
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The country in Europe that has marine west coast climate is Ireland
Explanation:
The marine west coast climate is one of the major climate types according to Koppen's climate classification. This climate type is mostly dictated by the sea. In Europe, the marine west coast climate can be found in a surprisingly high latitude, and the main reason for that are the warm ocean currents. The warm ocean currents of the Atlantic are running along the western coast of Europe, and they manage to have huge influence on the climate of the region.
- This climate type can be found at lower elevations and hills in Western Europe.
- The climate is warmer than it should be considering the latitude where this climate type is found in Europe.
- The summers are mild to warm, the springs and autumns mild to cold, while the winters are cold.
- The temperature extremes in both winter and summer are usually absent, and the climate is much more balanced.
- There is high amounts of precipitation throughout the whole year.
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Most El Nino climate patterns involve the Earth's atmosphere and the surface waters of the the Pacific Ocean<span>. El Nino is a climate cycle in the Pacific Ocean with a global impact on weather patterns. The cycle begins when warm water in the western tropical Pacific Ocean shifts eastward along the equator toward the coast of South America. Normally this warm water pools near Indonesia and the Philippines. During an El Nino, the Pacific's warmest surface waters sit offshore of northwestern South America. </span>
A convergent plate boundary is when two plates move towards each other, also known as a destructive plate boundary. So, the answer is A.
Answer: mid ocean ridges so I would go with the first one of at the spreading centers in the middle of the ocean
Explanation:
Not completely sure educated guess
