Switch thirsty crops, water by drip
Where most water goes to fields, moving from paddy and sugarcane to millets, pulses or maize, and from flood to drip or sprinkler irrigation, saves more than any recharge can add.
This area pumps out 1.5 times the water that rain puts back. That is the 2025 stage of groundwater extraction: water pumped out in a year as a share of what rain and other sources safely put back. Up 18 points since 2017.
Each point is one CGWB assessment. Over-exploited means more water leaves the ground than comes back, so the water table keeps falling. Hover over or tap a point to see why it moved.
| Year | Stage | Pumped out | Safe limit | Category | What changed |
|---|---|---|---|---|---|
| 2009 | 128.0% | 444 million m³ | 346 million m³ | Over-exploited | First assessment in this series. |
| 2013 | 124.0% | 469 million m³ | 379 million m³ | Over-exploited | Pumping up 6% (444 → 469 million m³). Safe limit up 9% (346 → 379 million m³). Main reason: more water soaked back into the ground, from better rain, canals or recharge structures. |
| 2017 | 134.6% | 605 million m³ | 450 million m³ | Over-exploited | Pumping up 29% (469 → 605 million m³). Safe limit up 19% (379 → 450 million m³). Main reason: more water was pumped out, mostly for irrigation (388 → 499 million m³). CGWB changed its method in 2017 (GEC-97 to GEC-2015), so part of this change comes from the new method. |
| 2020 | 187.1% | 642 million m³ | 343 million m³ | Over-exploited | Pumping up 6% (605 → 642 million m³). Safe limit down 24% (450 → 343 million m³). Main reason: less water soaked back in, from weaker rain, less canal seepage or more paved ground. |
| 2022 | 165.8% | 643 million m³ | 388 million m³ | Over-exploited | Pumping up 0% (642 → 643 million m³). Safe limit up 13% (343 → 388 million m³). Main reason: more water soaked back into the ground, from better rain, canals or recharge structures. |
| 2023 | 161.3% | 642 million m³ | 398 million m³ | Over-exploited | Pumping down 0% (643 → 642 million m³). Safe limit up 3% (388 → 398 million m³). Main reason: more water soaked back into the ground, from better rain, canals or recharge structures. |
| 2024 | 159.3% | 650 million m³ | 408 million m³ | Over-exploited | Pumping up 1% (642 → 650 million m³). Safe limit up 2% (398 → 408 million m³). |
| 2025 | 152.1% | 635 million m³ | 417 million m³ | Over-exploited | Pumping down 2% (650 → 635 million m³). Safe limit up 2% (408 → 417 million m³). Main reason: more water soaked back into the ground, from better rain, canals or recharge structures. |
Million m³: 1 million m³ = 100 crore litres. 2009 and 2013 used the older GEC-97 method.
Loading 20 years of rainfall…
175 of 940 water bodies (19%) are not in use: dried up, silted, built over or polluted. Bringing them back is one of the cheapest ways to recharge groundwater.
Loading the map of water bodies in Sawai Madhopur…
Source: 1st Census of Water Bodies, Ministry of Jal Shakti (counted in 2018-19, published 2023).
Most of the water here goes to farming, so using less on fields matters as much as recharge.
Where most water goes to fields, moving from paddy and sugarcane to millets, pulses or maize, and from flood to drip or sprinkler irrigation, saves more than any recharge can add.
Parks, campuses, warehouse yards and road sides can take recharge shafts that reach past the clay layer, so runoff that floods streets goes down to the aquifer instead.
Desilting old ponds and opening their feeder channels restores natural recharge. A one-hectare pond that soaks in a metre of water over the monsoon puts back about a crore litres.
Pipe roof water through a silt trap and filter into a recharge pit or an old borewell. Every 100 m² of roof puts back tens of thousands of litres a year, right where the pumping happens.
On sloping or rocky land, small dams on seasonal streams and trenches along contours slow water down long enough for it to sink in.
Treated water from a sewage treatment plant can run flushing, gardens, cooling towers and construction, which today often draw on borewells.
In the 2025 Central Ground Water Board assessment, Sawai Madhopur (Rajasthan) pumped out 152% of the groundwater that can be safely taken out each year, which puts it in the "over-exploited" category. That is 18 points higher than in 2017.
Yes. Sawai Madhopur takes out more groundwater than rain and other sources put back, so the water table keeps falling.
Rooftop rainwater harvesting into recharge pits or old borewells, recharge shafts in open land, reviving ponds, check dams, treating and reusing wastewater, and moving farms to drip irrigation and less thirsty crops.
The first Census of Water Bodies counted 940 water bodies in Sawai Madhopur, including 700 ponds. 175 of them were not in use.
Yearly rain at Sawai Madhopur, 2006–2025, from NASA satellite data. Lighter bars are dry years (20% or more below average), when wells are drawn hardest.
To stop the water table falling, Sawai Madhopur has to put back or save 218 million m³ a year. At 808 mm of rain, here is what that looks like:
In practice it is a mix: recharge in towns, ponds and check dams in villages, and saving water on farms and in factories.
1 mm of rain on 1 m² is 1 litre. The surface factor allows for water lost to splash, evaporation and first-flush.