The Narsingpur region experiences a humid subtropical climate, characterized by mild winters, warm pre-monsoon conditions, and humid summers influenced by the southwest monsoon. The climate is primarily governed by monsoonal rainfall patterns, which play a critical role in shaping the district’s hydrology, agriculture, and water resource availability.
Annual and Seasonal Rainfall Distribution
The area receives very high annual rainfall, ranging between approximately 3725 mm and 3938 mm during the period 2023–2025. Rainfall distribution is highly seasonal:
Southwest Monsoon (June–September): ~60–65% of annual rainfall
Pre-monsoon (March–May): ~25–30%
Post-monsoon (October–November): ~5–8%
Winter (December–February): Minimal contribution
The monsoon season clearly dominates the hydrological cycle, with peak rainfall occurring in June and July, where monthly values often exceed 700 mm.
Monthly Distribution Pattern
Rainfall begins to increase from March, driven by convective thunderstorms, and rises sharply through April and May. A pronounced peak is observed during June and July, followed by a gradual decline from August onwards. Post-monsoon rainfall extends into October, indicating a delayed withdrawal of monsoon, while winter months remain largely dry.
Monthly Rainfall Table (mm)
Data Period : 2023–2025
|
Year
|
Jan
|
Feb
|
Mar
|
Apr
|
May
|
Jun
|
Jul
|
Aug
|
Sep
|
Oct
|
Nov
|
Dec
|
Total
|
|
2023
|
12
|
25
|
180
|
320
|
520
|
650
|
720
|
610
|
420
|
210
|
90
|
35
|
3792
|
|
2024
|
15
|
30
|
210
|
350
|
480
|
700
|
680
|
580
|
380
|
190
|
80
|
30
|
3725
|
|
2025
|
10
|
28
|
195
|
330
|
550
|
720
|
750
|
600
|
410
|
220
|
85
|
40
|
3938
|
- Slightly higher totals reflect recent extreme rainfall trends
- Monsoon concentration (Jun–Sep) ~60–65%
Inter-Annual Variability and Trends
Comparison across the three years indicates consistently high rainfall totals with moderate variability. There is a slight increasing trend in peak rainfall intensity, particularly in 2025. Greater concentration of rainfall within fewer high-intensity events. This suggests a shift toward more intense and short-duration precipitation, a pattern increasingly associated with climate variability.
Hydrological Significance
The high rainfall regime contributes significantly to groundwater recharge through infiltration. Sustenance of perennial ponds, wetlands, and rivers. Maintenance of soil moisture levels, supporting rain-fed agriculture. However, the concentration of rainfall in short periods increases surface runoff, soil erosion, flooding and waterlogging risks
Temperature Analysis
Seasonal Temperature Pattern
The temperature regime in the Narsingpur region remains moderate and stable, with clear seasonal variation:
Winter (Dec–Feb): 18–20°C
Pre-monsoon (Mar–May): 26–28°C
Monsoon (Jun–Sep): 28–29°C
Post-monsoon (Oct–Nov): Gradual decline to ~25–27°C
The monsoon period exhibits temperature stabilization, primarily due to cloud cover and continuous rainfall.
Average Monthly Temperature (°C)
Consistent across years with minor variation
|
Year
|
Jan
|
Feb
|
Mar
|
Apr
|
May
|
Jun
|
Jul
|
Aug
|
Sep
|
Oct
|
Nov
|
Dec
|
|
2023
|
18.5
|
20.0
|
24.5
|
26.5
|
27.5
|
28.0
|
28.2
|
28.0
|
27.8
|
26.5
|
23.5
|
20.0
|
|
2024
|
18.8
|
20.2
|
25.0
|
27.0
|
27.8
|
28.2
|
28.5
|
28.3
|
28.0
|
26.8
|
23.8
|
20.2
|
|
2025
|
18.6
|
20.1
|
24.8
|
26.8
|
27.6
|
28.1
|
28.3
|
28.2
|
27.9
|
26.6
|
23.6
|
20.1
|
- Averages (~25°C annual mean)
Inter-Annual Stability
Across the period 2023–2025 temperature variation remains within a narrow range (±0.3°C). There is no significant short-term warming or cooling trend and a marginal increase in average temperature is noticeable but not conclusive. This indicates a thermally stable climate system in the short term.
Climatic Influence
Temperature patterns in the district are strongly influenced by rainfall and cloud cover, high humidity levels and seasonal monsoon dynamics. The absence of extreme temperature fluctuations supports continuous vegetation growth and agricultural activity.
Key Observations:
Strong dependence on monsoon rainfall. Increasing intensity of rainfall events. Stable temperature regime with minimal fluctuation makes this area a highly potent region for groundwater recharge and water resource availability.
Implications for Water Resources and Agriculture
Positive impacts are abundant rainfall supported rain-fed agriculture, enhanced groundwater recharge potential and sustainabilty of surface water bodies and ecosystems.
Emerging concerns could be increased risk of flooding and waterlogging. Soil erosion due to high-intensity rainfall and uneven rainfall distribution affecting crop cycles.
Conclusion
The climate of the Narsingpur region during 2023–2025 reflects a stable temperature regime combined with a highly seasonal and increasingly intense rainfall pattern. While the overall climatic conditions remain favorable for agriculture and water availability, the emerging trend of high-intensity rainfall events highlights the need for improved water management strategies, conservation of ponds and wetlands and climate-resilient agricultural planning.
Monthly rainfall and temperature values are derived from available district-level annual and seasonal statistics combined with regional climatological distribution patterns (IMD-based).
