Quantification of rainfall, temperature, and reference evapotranspiration trend and their interrelationship in sub-climatic zones of Bangladesh.

Also, the annual season exhibited a negative trend in both zone C (−0.56 mm/year) and zone E (−0.76 mm/year), along with the addition of zone D (−0.61 mm/year).

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Conversely, a different pattern is noticed during the post-monsoon season, with a rising trend observed in the southern and south-eastern parts, particularly where only zone A demonstrates a positive trend of 1.18 mm ( Fig. 3 and Table 1 ).

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However, zone A exhibited a decreasing trend in minimum temperature during the winter and pre-monsoon seasons ( Table 1 ).

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In the north-eastern zone, a significant trend (4.36 °C) in the minimum temperature during the monsoon season was confirmed by a slope of 0.02 °C/year.

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Similarly, an increasing trend was observed in monsoon rainfall for zone A, with a value of 0.11 mm for the annual season.

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