By Prabhu Mallikarjun
Tamil du and Kartaka’s Cauvery basin reservoirs are half as full as they should be, according to an IndiaSpend alysis of reservoir data in both states, even as the Supreme Court modified its week-old order and allowed Kartaka to release 20 per cent less water — 12,000 cubic feet per second, or cusecs, per day for the next eight days.
Violence erupted on September 12 in both states after the Supreme Court order. Both states are short of water — with a “normal” monsoon masking local rainfall deficits — and the data indicate there is no option but to share the Cauvery’s water. Variations in rainfall are likely to grow, part of changes that scientists are recording in local and global weather.
Overall, Kartaka’s reservoirs were 30 per cent short of water, compared to 49 per cent in Tamil du, according to Central Water Commission data, as on September 8. But the capacity of Cauvery basin reservoirs in Kartaka is a quarter less than Tamil du’s, 2.75 billion cubic meters (BCM), against 3.44 BMC in Tamil du.
Water levels of the main reservoirs in the Cauvery catchment area of Kartaka and Tamil du — including the Krish Raja Sagara (KRS) dam in Mandya district, Kabini in Mysore, Harangi in Kodagu and Hemavathi in Hassan; Mettur dam in Salem and Bhavanisagar Dam in Erode — were, together, 46 per cent less than normal (based on a 10-year average) and 27 per cent less than the levels in 2015 (except Harangi), according to CWC data.
The situation in four other reservoirs of Tamil du was no better. Vagai in Theni district was at 5 per cent of capacity; the Parambikulam dam in Kerala (operated by Tamil du) was at 41 per cent of capacity; Aliyar dam in Coimbatore was at 9 per cent of capacity; and the Sholayur dam, also in Coimbatore, was at 49 per cent of capacity.
Water in the reservoirs of the two feuding states must now be shared between not just farmers but cities as drinking water and for hydel power.
The post-monsoon season of discontent in both states is a consequence of rainfall variation masked by a monsoon declared as “normal”.
While Kartaka was 17 per cent short of normal rainfall between June 1 and September 9 — the meteorological department classifies this as a “normal” deficit, but rainfall was intermittent and uncertain through the monsoons — Tamil du recorded normal rainfall, according to data from the Kartaka State tural Disaster Monitoring Centre (KSNDMC) and the Indian Meteorological Department (IMD), respectively.
Tamil du received 222 mm rainfall, against the normal of 223 mm rainfall till September 9. Kartaka recorded 594 mm rainfall against the normal of 718 mm over the same period.
Apart from half-full reservoirs in the Cauvery catchment area, 42 per cent of Kartaka’s minor irrigation tanks are dry statewide and 90 per cent of Kartaka’s talukas — subdivisions of districts — recorded deficit rainfall in August.
Local rainfall deficits in both states is not classified as a meteorological drought (reduction in rainfall for a specific period), but it has resulted in an agricultural drought (when rainfall and soil moisture are idequate during the crop-growing season). The result: Reduced and delayed sowing in many districts of both states.
For instance, in August, Mandya was classified as having received “excess” rainfall. Yet, sowing was reported to be less than a quarter of normal. This was because until the last day of the month, Mandya recorded less than 1 mm rainfall daily (except on August 27 and August 30), against the daily normal of 2-3 mm. On August 31, Mandya recorded 34 mm rainfall, increasing the month’s average.
Similar trends were observed in the other Cauvery basin districts of Kartaka, including Mysuru, Chamarajagar and Ramagara. No public data are available for Tamil du’s districts in the Cauvery delta.
However, Tamil du’s Cauvery basin districts of Erode, Salem, Karur, Trichy and Thanjavur received “normal” rainfall (0 to 12 per cent excess compared to normal), according to IMD data.
“The state’s (Kartaka) rainfall is not decreasing at all,” said Shivaramu H.S., professor and head of Agro-Meteorology Department, University Of Agricultural Sciences, Bengaluru. “But the number of rain days is coming down. This results in run-off causing rain (rain with high intensity) which is not good in the long run. With run-off causing rain, lots of nutrients are drained away, lots of silt gets drained away, and fertile soil becomes barren.”
Extreme rainfall events in central India, the core of the monsoon system, are increasing and moderate rainfall is decreasing — as a part of complex changes in local and world weather — according to a clutch of Indian and global studies reviewed by IndiaSpend in April 2015. These variations are evident in south India too.
“There is a spatial disturbance in the rainfall pattern,” said Shivaramu. “In the Cauvery basin and Kodagu, rainfall is decreasing almost 2 mm per year in the long run. But in Bengaluru, Kolar, Chikkaballapura and Ramagara, rainfall is increasing at 1 mm per annum.”
Apart from coping with growing variations, a long-term solution is not easy. About 2,000 thousand million cubic feet (TMC) of water from Kartaka’s west-flowing rivers drains into the Arabian Sea every year. That is four times as much as the water requirements of both states put together. “If the Government can find a way to harness this in the long run, then we won’t have to fight for Cauvery every year,” said A.C. Kamaraj, chairman, tiol Waterways Development Technology.
(In arrangement with IndiaSpend.org, a data-driven, non-profit, public interest jourlism platform. Prabhu Mallikarjun is a Bengaluru-based independent reporter and a member of 101Reporters.com, a pan-India network of grassroots reporters. The views expressed are those of IndiaSpend. Feedback at email@example.com)