Analysis of Climate Factors: Precipitation, Temperature, and Aridity
Classified in Geology
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Analysis of Precipitation
Total Precipitation
- Very abundant: +1000 mm (mountain climate)
- Abundant: +800 mm (oceanic climate)
- Short: 800-300 mm (continentalized coastal Mediterranean climate)
- Very low: <300 mm (sub-desert steppe climate)
- Extremely low: <150 mm (desert climate)
Distribution of Rainfall
- Regular: No dry month with rainfall < 30 mm (oceanic climate)
- Fairly regular: Maximum of 2 dry months (oceanic climate transitioning towards continental Mediterranean)
- Irregular: More than 2 dry months (Mediterranean climate), +7 dry months (dry sub-desert or steppe Mediterranean climate)
Noteworthy points:
- Seasons with more abundant precipitation
- Months with less or no rainfall (dry months)
Analysis of Temperature
Average Annual Temperature and Thermal Amplitude
Thermal amplitude: The difference between the warmest and coldest month.
Coastal Areas
- Very low: <8°C (Canary Islands)
- Low: 9-12°C (Cantabrian coast)
- Average: 12-16°C (Mediterranean and South Atlantic coast)
Inland Areas
- High: 16-18°C
- Very high: >18°C
Summer Temperature
- Warm: ≥22°C
- Cool: <22°C
Winter Temperature
- Mild: ≥10°C
- Moderate: 6-10°C
- Cold: 3-6°C
Mountain climates have winter temperatures below 0°C.
Aridity Analysis
Relationship between precipitation and temperature.
Monthly Aridity
Determined using the Gaussen Index (2T°C > P mm) or by observing if the temperature curve on a climograph is above the precipitation bars. Since the rainfall scale is twice the temperature scale, this indicates a dry month according to the Gaussen Index.
- Oceanic climate: No dry month
- Transitional oceanic climate: Maximum of 2 dry months
- Mediterranean climate: +2 dry months
General Aridity
- Humid: No dry month
- Semi-humid: 1-3 dry months
- Semi-arid: 4-6 dry months
- Extreme semi-arid: 7-11 dry months
Climate Classification
Analyze all previous data to determine the climate type.
Geographical Location
Consider the thermal amplitude.