Course Content
Crop Production (Unit 6)
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ASRB NET / SRF / Ph.D. Agronomy
Rainfall Analysis and Length of Growing Season (LGS)

 

  1. 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.

 

 

  1. 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.
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