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Climate and rainfall: why Marathwada is dry

The Konkan is among the wettest regions of India; a few hundred kilometres east, parts of Marathwada and western Maharashtra struggle for drinking water in May. The reason is a mountain range and a wind. How Maharashtra's climate works, region by region.

7 Oct 2026 5 min read

In this guide
  1. Maharashtra's climate type
  2. How the monsoon reaches Maharashtra
  3. Regional rainfall
  4. Why Marathwada is dry
  5. Temperature
  6. Implications
  7. Climate change
  8. Practice
  9. A one-page summary

In July, the ghat roads between Mumbai and Pune are wrapped in cloud, with waterfalls pouring off every cliff. Drive a few hours further east, and you may find farmers in Solapur, Beed or Dharashiv anxiously watching an empty sky. The contrast is not bad luck. It is the result of how the monsoon meets the Sahyadri — and it explains more about Maharashtra's economy and politics than almost any other geographical fact.

Maharashtra's climate type

Maharashtra has a tropical monsoon climate. The year divides into:

SeasonMonths (approx.)Features
SummerMarch – MayHot and dry; very high temperatures in Vidarbha
South-west monsoonJune – SeptemberMost of the year's rainfall
Retreating monsoonOctober – NovemberSome rain, especially in the south; thunderstorms
WinterDecember – FebruaryCool and dry; cold nights in the interior

The south-west monsoon brings the bulk of Maharashtra's annual rainfall — typically the large majority of the year's total.

How the monsoon reaches Maharashtra

The south-west monsoon arrives in two branches:

  1. The Arabian Sea branch — reaches the Konkan coast, usually in early June. It strikes the Sahyadri head-on.
  2. The Bay of Bengal branch — reaches eastern Vidarbha from the east and north-east.

Orographic rainfall and the rain shadow

When the moist Arabian Sea winds hit the Sahyadri, they are forced to rise. As they rise, they cool, and their moisture condenses into heavy rain on the windward (western) slopes. This is orographic or relief rainfall.

By the time the winds cross the crest and descend on the leeward (eastern) side, they have lost much of their moisture, and as they descend they warm, which reduces the chance of rain further. The area immediately east of the Sahyadri is therefore a rain shadow region.

Regional rainfall

RegionTypical rainfallNotes
Konkan coastVery high (generally well above 2,000 mm)Heaviest along the southern Konkan and the ghat slopes
Sahyadri crest and ghatsExtremely highPlaces such as Amboli and Mahabaleshwar receive some of the heaviest rain in the state
Rain shadow belt (east of the Sahyadri: parts of Pune, Satara, Sangli, Solapur, Ahilyanagar, Beed, Dharashiv)Low (often under 600–700 mm)The most drought-prone region
MarathwadaLow to moderate, and erraticFrequent dry spells; the core of Maharashtra's drought problem
Western Vidarbha (Amravati, Akola, Buldhana, Washim, Yavatmal)ModerateCotton belt; vulnerable to dry spells
Eastern Vidarbha (Nagpur, Bhandara, Gondia, Chandrapur, Gadchiroli)Moderate to highBay of Bengal branch; rice cultivation and tanks

The exact figures vary by source and year; learn the pattern — very high on the coast and ghats, lowest in the rain shadow, rising again towards eastern Vidarbha.

Why Marathwada is dry

Marathwada's dryness has several causes:

  1. Rain shadow: it lies in the lee of the Sahyadri.
  2. Distance from both monsoon branches: it is too far east to benefit from the Arabian Sea branch and too far west to receive much from the Bay of Bengal branch.
  3. Erratic monsoon: rain often comes in a few heavy spells separated by long dry periods, which is worse for crops than steady rain.
  4. High evaporation: hot temperatures increase evaporation from soil and reservoirs.
  5. Soil and geology: basalt has limited capacity to store groundwater, so recharge is poor.

Human factors make it worse: water-intensive crops such as sugarcane, over-extraction of groundwater, and deforestation.

Temperature

  • Konkan: moderate temperatures throughout the year because of the sea's influence; high humidity.
  • The plateau: hot summers; cool, dry winters. Pune and Nashik have relatively pleasant climates because of their elevation.
  • Vidarbha: extreme. Cities such as Chandrapur, Brahmapuri, Nagpur, Akola and Wardha regularly record summer temperatures among the highest in India, often above 45 °C.
  • Hill stations: Mahabaleshwar, Matheran, Chikhaldara and Toranmal are cooler.

Heatwaves in Vidarbha and Marathwada are a growing public-health concern.

Implications

For agriculture

  • Kharif crops (June–October) depend on the monsoon: rice, soybean, cotton, jowar, bajra, tur, moong.
  • Rabi crops (winter) depend on residual moisture and irrigation: wheat, rabi jowar, gram.
  • In the rain shadow, farmers rely on drought-tolerant crops (jowar, bajra, pulses) unless irrigation is available.

For water management

  • Heavy rain in a short season, followed by months of dryness, makes storage essential — dams, tanks, farm ponds and groundwater recharge.
  • The mismatch between where rain falls (Konkan, ghats) and where water is needed (plateau) drives proposals for river linking and inter-basin transfers.

For disasters

  • Floods and landslides in the Konkan and ghats during intense rain (for example, Taliye in Raigad, 2021).
  • Drought in the rain shadow and Marathwada.
  • Heatwaves in Vidarbha.

Climate change

Studies suggest the monsoon in Maharashtra is becoming more variable, with more extreme rainfall events and longer dry spells. The state has a State Action Plan on Climate Change. This makes drought-proofing, flood management and climate-resilient agriculture central to development. See our guide on climate change and Maharashtra.

Practice

Prelims-style:

  1. What causes heavy rainfall on the western slopes of the Sahyadri?
  2. Which branch of the monsoon brings rain to eastern Vidarbha?
  3. Name three districts in the rain shadow region.
  4. Why does the Konkan have moderate temperatures throughout the year?

Mains-style:

  • "Marathwada's water crisis is as much man-made as natural." Discuss.
  • Explain the climatic basis of regional disparities in agriculture in Maharashtra.

A one-page summary

Draw a west–east cross-section of Maharashtra: the sea, the Konkan, the Sahyadri, the rain shadow, the plateau, Vidarbha. Mark the monsoon wind rising on the west, raining, and descending dry on the east. Add rainfall labels. If you can draw and explain this diagram in two minutes, you can answer almost any climate question MPSC asks.

A note on dates and numbers. Exam patterns, vacancies and schedules change from year to year. Always confirm the current details in the latest notification on the Maharashtra Public Service Commission website .

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