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Westmanna has less yearly range in temperature compared to Hebron because Westmanna is located on an island, which tends to have a moderating effect on temperatures due to the surrounding ocean. Hebron, on the other hand, is inland and further from any moderating influences, leading to greater temperature fluctuations throughout the year.

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1y ago

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What is the avg yearly rainfall in Australia?

The average yearly rainfall in Australia varies widely across the country. The northern parts of Australia receive higher average rainfall, with areas like the tropical north averaging around 2,000 mm per year. In contrast, southern and central regions tend to have lower average rainfall, with some areas receiving less than 300 mm per year.


Why the yearly total precipitation over the oceans is greater than the yearly total precipitation over the continents?

The yearly total precipitation over the oceans is greater than over continents because oceans cover more of the Earth's surface and therefore have a larger area from which to receive precipitation. Additionally, the oceans are able to retain heat better than land, leading to more evaporation and subsequent precipitation. Ocean currents also play a role in transporting moisture to different regions, contributing to higher precipitation levels over oceans.


Why does one side of a mountain range have significantly less precipitation than the other side?

One side of a mountain range will have significantly less precipitation than the other side due to the height of the mountain. The clouds that carry the water for precipitation, may be blocked by the tall mountains.


How much does it rain in 1 year?

The average global yearly rainfall is about 1000 mm (39 inches). However, this can vary significantly depending on the region, ranging from less than 100 mm in arid areas to over 10,000 mm in some tropical regions.


How does the Great Dividing Range affect Australia's climates?

More rain comes to the range that is in line with the wind. Air starts to rise when it begins to come in contact with the Dividing Range. The opposite side or the side without the prevailing range receives less rainfall as a result. Air is falling rather than rising on this side of the range. Which side of the range either has or does not have the prevailing range will either receive a lot of rainfall or very little.