Abstract


 Analysis of long-term rainfall data (1986-2018) of Bastar region revealed decreasing trend in total quantum of annual rainfall with varying frequency and distribution. The quantity of winter and summer rains decreased drastically during 2008-18 as compared to earlier two decades (1986-96 and 1997-2007). SW monsoon rain of 2008-18 was more than past two decades, whereas NE monsoon rain changed much in quantity except during 1997-2007. During 1986-96, the pre-monsoon shower was received in April, but later two decades the shower was received in May, which supports for summer ploughing and dry aerobic seeding. The cropping period almost synchronized between 22-43 standard meteorological week (SMW) reaching 93.11 mm per week as maximum rainfall. As the probability of 20 mm rainfall decreased from 75 to 50%, the crop yield got reduced by 30%. The mid-land rice with a probability of 13.47 to 16.07 mm rain per week supported growth phase during 17-21SMW. Whereas, upland rice maturing in 90-100 days could avoid dry spells, if the rice is managed by conservation furrows at the time of sowing. The summer ploughing is preferred with more than 40 mm rain in single day during March to April for mitigating dry spells. On the other hand, preparatory tillage and sowing were performed together in support of ripening niger and horsegram under probability of 75, 50 and 25% rain through crop planning. Maize and small millets reduced yield significantly when rainfall reached 75% deficit, whereas 25% deficit rain did not affect the yields.

Highlights

  • Rainfall is crucial in agricultural planning for rainfed region which completely depends on rainfall and its distribution in any annual calendar

  • Bastar region received more than 1000 mm annual rainfall whereas the years1997 and 2002 received less than 1000 mm

  • Rainfall distribution was divided in three parts as 1to 23 (I), 24to 36 (II) and 37to 50 (III) standard meteorological weeks (SMW) in which mean, standard deviation and co-efficient of variation were highlyfluctuated in I and III part

Read more

Summary

Introduction

Rainfall is crucial in agricultural planning for rainfed region which completely depends on rainfall and its distribution in any annual calendar. The change in rainfall can’t be assessed due process of cloud formation and raining is unpredictable, but long-term rainfall analysis could be scaled up the planning of agriculture in rainfed region. Urd and moong are very much affected by rainfall trend in the region due to early down pour, mid-season and terminal drought. The arhar crop falls under terminal drought whereas remaining two crops i.e., urd and moong coincide with heavy shower and waterlogged condition. This harsh situation changed the land use pattern of the region. The existing scenario of the long-term rainfall has been considered under study to fulfil the objective of crop planning based on rainfall trend

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call