The charts below show temperature and rainfall in Equatorial climate and Mediterranean climate

1. Graph Types: Column graphs

2. Title: Temperature and Rainfall in Equatorial and Mediterranean Climates

3. What are the units of measurement?: Millimeters (mm) for rainfall and degrees Celsius (°C) for temperature

4. Who: Climatologists, environmental scientists, or anyone studying climate patterns

5. When: Not specified (data for unspecified months in a year)

6. Where: Equatorial and Mediterranean regions

7. Topic: Comparison of temperature and rainfall in two different climates

•  Equatorial Climate:
•  Wettest months are November, December, and January, with rainfall between 230 and 270 mm.
•  Rainfall in other months fluctuates between 180 and 190 mm, indicating consistent precipitation throughout the year.

•  Mediterranean Climate:
•  Maximum rainfall occurs in January at around 170 mm, followed by December at 150 mm.
• February, March, and November receive moderate rainfall (70–90 mm), while other months are relatively dry, with rainfall below 20 mm.

• Equatorial Climate:
• Temperature remains stable year-round, ranging from 24°C to 26°C, with May and June slightly hotter.

• Mediterranean Climate:
• Starts at around 11°C in January, gradually rising to a peak of 28°C in August, before dropping back to 11°C by December.

The column graphs illustrate the temperature and rainfall patterns of Equatorial and Mediterranean climates.

 In the Equatorial climate, the rainfall is notably higher, with the wettest months being November, December, and January, experiencing between 230 mm and 270 mm of rain. The temperature remains relatively stable throughout the year, consistently ranging between 24°C and 26°C, with minor peaks in May and June.

 Conversely, the Mediterranean climate exhibits a marked seasonal variation in both temperature and rainfall. The highest rainfall is recorded in January at around 170 mm, while the driest months see rainfall levels below 20 mm. Temperature ranges from a low of 11°C in January to a high of 28°C in August, demonstrating a significant fluctuation across the seasons.

 In conclusion, the Equatorial climate is characterized by higher temperatures and consistent rainfall, while the Mediterranean climate is cooler and experiences more pronounced seasonal variations in both temperature and precipitation.

The column graphs compare temperature and rainfall in two distinct climates: Equatorial and Mediterranean.

Overall, cooler temperatures and lower rainfall characterize the Mediterranean climate compared to the Equatorial climate, which features consistently high temperatures and abundant precipitation year-round.

In the Equatorial climate, November, December, and January are the wettest months, with rainfall reaching between 230 mm and 270 mm. In contrast, rainfall in the remaining months fluctuates between 180 mm and 190 mm, demonstrating a consistent precipitation pattern throughout the year. The temperature in this climate is fairly stable, ranging from 24°C to 26°C, with May and June slightly warmer than the rest of the months.

The Mediterranean climate experiences its highest rainfall in January, measuring around 170 mm, followed by December at 150 mm. February, March, and November have moderate rainfall, ranging from 70 mm to 90 mm, while the other months are relatively dry, with rainfall levels dropping below 20 mm. The temperature in the Mediterranean climate starts at approximately 11°C in January, gradually increasing to a peak of 28°C in August before falling back to 11°C by December.

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