Rainfall Analysis and Length of Growing Season (LGS)
- Rainfall Analysis
Definition: Rainfall analysis is the study of the amount, distribution, and variability of rainfall over time to understand its impact on crop production and water availability in drylands.
Purpose:
- To determine the suitability of crops for an area.
- To plan sowing dates, cropping patterns, and moisture management strategies.
- To assess drought risk and crop failure probability.
Key Parameters of Rainfall Analysis
Parameter |
Description |
Significance in Drylands |
Annual Rainfall (AR) |
Total rainfall in a year (mm) |
Determines dryland classification |
Monthly/Seasonal Rainfall |
Distribution of rainfall by months or seasons |
Identifies critical crop growth periods |
Rainfall Variability (CV%) |
Coefficient of variation = (Standard deviation ÷ Mean) × 100 |
High CV → greater drought risk |
Probability of Dry Spell |
Frequency of periods with < 5 mm/day rainfall |
Helps in planning irrigation/fallowing |
Onset & Withdrawal of Monsoon |
Dates of first and last effective rains |
Determines sowing and harvesting dates |
Facts:
- Rainfall less than 500 mm/year: Arid areas (high risk, dry farming).
- Rainfall 500–1000 mm/year: Semi-arid areas (dryland farming).
- Rainfall 1000–1150 mm/year: Dry sub-humid areas (rainfed farming).
- Southwest monsoon contributes ~70% of rainfall in drylands.
- CV of rainfall: 20–60% in semi-arid/arid zones → high drought probability.
Methods of Rainfall Analysis:
- Statistical methods: Mean, standard deviation, coefficient of variation, probability of exceedance.
- Water balance approach: Compare rainfall with potential evapotranspiration (PET) to assess moisture availability.
- Rainfall threshold analysis: Minimum rainfall required at critical crop growth stages.
- Length of Growing Season (LGS) / Length of Growing Period (LGP)
Definition: LGS is the period (in days) during which soil moisture is adequate for the growth of crops without supplemental irrigation.
Significance:
- Determines crop selection and cropping system in drylands.
- Short LGS → need for short-duration, drought-tolerant crops.
- Long LGS → possible multiple cropping or intercropping.
Classification of LGS in Drylands
Zone |
LGS (days) |
Crops Suitable |
Arid |
< 90 |
Pearl millet, moth bean, cluster bean |
Semi-Arid |
90–150 |
Sorghum, pigeon pea, sunflower, groundnut |
Dry Sub-Humid |
150–180 |
Rice, maize, soybean, pulses |
Factors Affecting LGS:
- Rainfall onset and distribution – irregular rains shorten LGS.
- Soil water-holding capacity – sandy soils → shorter effective LGS.
- Evapotranspiration (ET) – high ET reduces effective moisture.
- Temperature – very high or very low temperatures affect crop growth.
Facts:
- Drylands of India have LGS ranging from <90 days (arid) to 180 days (dry sub-humid).
- LGS is shorter than total calendar season due to mid-season droughts and uneven rainfall.
- Short LGS crops are mostly millets, pulses, and drought-tolerant oilseeds.
Relationship Between Rainfall Analysis & LGS
- Rainfall amount & distribution → Determines LGS.
- Erratic rainfall → Shortens effective LGS, increasing risk of crop failure.
- LGS is used in agro-climatic zoning, crop planning, and risk assessment.
Quick Facts for ASRB NET:
- Arid (<500 mm rainfall): LGS <90 days → pearl millet, moth bean.
- Semi-arid (500–1000 mm rainfall): LGS 90–150 days → sorghum, pigeon pea, sunflower.
- Dry sub-humid (1000–1150 mm rainfall): LGS 150–180 days → rice, maize, soybean.
- LGS helps in delineating dryland tracts for research and crop management.
Distribution of Rainfall in India
Feature |
Details |
Average Annual Rainfall |
~1170 mm (varies widely across regions) |
Monsoon Contribution |
Southwest Monsoon (June–Sept) → ~70% of annual rainfall |
Northeast Monsoon (Oct–Dec) |
Contributes mainly to Tamil Nadu, Kerala, and southeastern states |
Regional Variation |
Arid (<500 mm) → Rajasthan, western Gujarat |
Semi-arid (500–1000 mm) → Deccan Plateau, Bundelkhand |
|
Sub-humid/Dry sub-humid (1000–1150 mm) → Eastern UP, Bihar, Odisha |
|
Humid (>1150 mm) → Western Ghats, NE India |
|
Extreme Rainfall |
Cherrapunji & Mawsynram (~11,000–12,000 mm) |
Facts:
- India’s rainfall is highly spatially and temporally variable.
- Coefficient of variation (CV):
- Arid/semi-arid → 20–60% (high risk of drought)
- Humid regions → <20% (more reliable rainfall)
Temporal Distribution
- Southwest Monsoon (June–Sept): Major rainfall contributor (~70% of annual rainfall).
- Northeast Monsoon (Oct–Dec): Important for Tamil Nadu, Kerala, Andhra Pradesh.
- Pre-Monsoon & Post-Monsoon Showers: Minor contribution; help in sowing summer crops.
Facts:
- Late onset or early withdrawal of monsoon → shortens effective growing season.
- Mid-season dry spells → reduce yield by 20–50% in rainfed areas.
Effective Rainfall
- Definition: Portion of total rainfall available for crop use after losses due to runoff, deep percolation, evaporation.
- Fact: Effective rainfall in arid regions <300 mm, even if total rainfall = 500 mm.