When studying climate which of the following would be considered an example of the macro scale level?

What are the two weather variables used most often as indicators of climate?

The two weather variables used most often as indicators of climate are: precipitation and temperature.

How do we classify climate?

Weather Patterns

Long-term records of temperature and precipitation reveal climate patterns across continents, delineating them into climate regions. … Class names for classification systems based on weather patterns often include geographical names such as polar, tropical, continental, and marine.

What two atmospheric elements are most often used when classifying climates?

The most familiar features of a region’s climate are probably average temperature and precipitation. Changes in day-to-day, day-to-night, and seasonal variations also help determine specific climates. For example, San Francisco, California, and Beijing, China, have similar yearly temperatures and precipitation.

What are climate variables?

Climate entails the statistical characteristics of weather conditions in a given area. Climate zones are characterized by different combinations of climate variables, such as temperature, precipitation, humidity, and wind.

What are some examples of weather?

Weather includes sunshine, rain, cloud cover, winds, hail, snow, sleet, freezing rain, flooding, blizzards, ice storms, thunderstorms, steady rains from a cold front or warm front, excessive heat, heat waves and more. … They also provide Special Weather Statements and Short and Long Term Forecasts.

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What is the need of climate classification?

Climate classification is an important variable when studying health-related effects as climate determines many facets of season. For example, some climates only experience two principle seasons (e.g., wet vs dry season) while others experience the more traditional ‘four season’ climate.

What kind of data do scientists use to study climate?

When scientists focus on climate from before the past 100-150 years, they use records from physical, chemical, and biological materials preserved within the geologic record. Organisms (such as diatoms, forams, and coral) can serve as useful climate proxies.