Maharashtra is again approaching a water crisis, with a reported 18% rainfall deficit, prolonged dry spells and the possibility of drought-like conditions across 21 districts. The immediate damage is visible in scorched standing crops and falling well levels, but the larger concern is institutional: the state is once again being pushed to manage drinking water, livestock, agriculture and the next farming season with increasingly limited reserves.
The report published by Loksatta on September 25 says the current situation may be more serious than several drought-like and drought conditions recorded during the past decade. The assessment is not that an official drought has already been declared across the state. Rather, it points to a widening risk, particularly in Marathwada, where reservoir storage had fallen to about 46% by September.
That distinction matters. Drought is not determined only by whether rainfall is below normal. Administrative declarations also influence the release of relief, the identification of affected talukas and villages, and the deployment of measures for drinking water, fodder and agriculture. A drought-like condition can therefore represent a period when households and farms are already under pressure, even before the full official process is completed.
The present episode has been intensified by the timing of the rainfall deficit. The report says that large breaks in rainfall continued into the second half of September, leaving many areas without adequate rain even as the kharif season progressed. Standing crops have been damaged, groundwater levels have fallen and the shortage of drinking water and fodder has become more acute. The state is now preparing water arrangements for affected farmers, people dependent on drinking-water supplies, livestock and the coming rabi season.
The pattern is not new. According to the report, Maharashtra has faced six significant water-stress episodes in the past 12 years: two periods described as drought-like, one period of severe water scarcity, two officially declared droughts and one limited drought. The recurrence raises a question beyond this year’s rainfall: whether the state’s water system is being managed as a sequence of emergencies rather than as a long-term allocation and storage problem.
The clearest historical warning came in 2015. Average rainfall that year was reported at only 59.4% of normal, while rainfall deficiency was recorded in 278 of the state’s 355 talukas. Eleven years ago, in the same month, the crisis in Latur became so severe that water had to be transported by railway wagons. That episode remains a powerful reminder that a rainfall shock can quickly become a logistics and public-administration crisis when local sources and reserves are unable to meet demand.
The 2018-19 drought showed how widely the consequences can spread. The state declared a drought in 159 talukas, including 112 classified as severely affected and 39 as moderately affected. Around 85.76 lakh hectares were reported to have been affected. The government also had to identify drought-like conditions across revenue circles and villages, widening the administrative geography of the response.
A limited drought was declared in 2019-20, followed by another official drought episode in 2023-24. During the 2023 kharif season, drought was declared in 40 talukas across 15 districts. Of these, 24 talukas were classified as severely affected and 16 as moderately affected. About 22.66 lakh hectares were affected, and the state government approved assistance of approximately Rs 2,443 crore.
These figures show that the scale of impact can vary sharply between episodes. The 2018-19 crisis covered a much larger reported area than the 2023-24 episode, while the current report focuses on a possible spread across 21 districts and a significant rainfall deficit. The comparison also shows why district and taluka-level classification is central to water governance. Statewide rainfall averages can conceal major differences in local rainfall, storage, crop exposure and access to drinking water.
Reservoir storage is another critical part of the picture. The reported 46% storage level in Marathwada by September indicates that the region’s water position cannot be assessed only through rainfall totals. What matters for households and farms is whether water stored in reservoirs, wells and local sources can last through the remaining agricultural season and support drinking-water needs. The same reserves may also be required for the rabi crop, creating competing demands within the same hydrological cycle.
This is where water scarcity becomes an infrastructure and governance issue. Reservoirs, canals, pipelines, wells and tanker systems are not separate responses; together they form the delivery system through which water reaches settlements, farms and livestock. When rainfall is delayed or interrupted, the performance of that system determines whether a meteorological deficit becomes a local emergency. The report’s reference to falling well levels and drinking-water concerns suggests that both surface and groundwater sources are under pressure.
The administrative response is also likely to determine how quickly affected areas receive support. Drought declarations, classifications of severity and assistance packages create the framework for relief, but the report does not establish the final list of affected districts, the detailed allocation of resources or the operational timetable for water supply measures. Those are important pending details because the current assessment describes a possible expansion of drought-like conditions rather than a completed statewide declaration.
The recurrence of crisis also complicates agricultural planning. Kharif crops have already suffered from the prolonged break in rainfall, while the state must now plan water availability for rabi cultivation. Decisions over how much water can be released for farming, drinking and livestock will be made under conditions of uncertainty. The report confirms that the government has begun preparing for these competing needs, but it does not provide the final water-allocation plan or identify the specific measures that will be implemented in each district.
For cities and towns, the issue is not confined to rural areas. The same state-level water system connects reservoirs, regional supply networks and local distribution arrangements. When water sources weaken, the pressure can move through administrative boundaries, affecting the reliability of supply and increasing dependence on emergency arrangements. The Latur railway-water episode demonstrated how a local shortage can require a large-scale transport response. The present report does not say that such a response is now required, but it shows why reservoir and groundwater trends matter beyond individual farms.
The evidence currently supports three conclusions. First, Maharashtra is facing a serious rainfall and water-stress episode, with a reported 18% rainfall deficit and particularly severe concern in Marathwada. Second, the state has repeatedly moved through drought-like or officially declared drought conditions over the past 12 years, with substantial effects on talukas, villages, crops and public finances. Third, the immediate response is being shaped by the need to balance drinking water, livestock, damaged kharif crops and the upcoming rabi season.
What remains uncertain is the final administrative status of the 21 districts, the extent of assistance that will be approved and whether reservoir and groundwater conditions will improve before the next critical demands emerge. Those decisions, along with the government’s district-level water planning, will determine whether this episode remains a drought-like warning or develops into another formally declared statewide water crisis.
