Nirmāli Weather Today

Climate and Weather in Nirmali, IN

Nirmali is a small town located in the Supaul district of the Indian state of Bihar. It is known for its rich cultural heritage and historical significance. The town experiences a subtropical climate with distinct seasons throughout the year. In this article, we will explore the weather patterns in Nirmali and provide a comprehensive overview of its climate.

Temperature

Nirmali experiences a wide range of temperatures throughout the year, with hot summers and cool winters. The average annual temperature in Nirmali is around 25 degrees Celsius (77 degrees Fahrenheit). Let's take a closer look at the temperature variations in different seasons:

Summer (March to June):

The summer season in Nirmali is characterized by high temperatures and scorching heat. The average maximum temperature during this time ranges from 35 to 40 degrees Celsius (95 to 104 degrees Fahrenheit), with occasional heatwaves pushing the mercury even higher. The nights are relatively cooler, with temperatures dropping to around 25 degrees Celsius (77 degrees Fahrenheit).

Monsoon (July to September):

The monsoon season in Nirmali brings relief from the summer heat with moderate to heavy rainfall. The average rainfall during this period is around 1000 mm, which contributes significantly to the region's agricultural productivity. The temperatures during the monsoon season range from 30 to 35 degrees Celsius (86 to 95 degrees Fahrenheit), with high humidity.

Winter (October to February):

Winter in Nirmali is relatively mild and pleasant, with cool temperatures. The average minimum temperature during this season ranges from 10 to 15 degrees Celsius (50 to 59 degrees Fahrenheit), while the maximum temperature hovers around 20 to 25 degrees Celsius (68 to 77 degrees Fahrenheit). The region experiences a moderate level of fog during the winter months, which can occasionally disrupt transportation.

Rainfall

Nirmali receives the majority of its annual rainfall during the monsoon season, which lasts from July to September. The region experiences an average annual rainfall of around 1000 mm. The monsoon showers play a crucial role in nourishing the agricultural fields and contributing to the overall prosperity of the region. However, excessive rainfall can sometimes lead to flooding and waterlogging in low-lying areas, causing temporary disruptions.

Wind Patterns

The wind patterns in Nirmali are influenced by the seasonal changes and the surrounding geographical features. During the summer season, hot and dry winds from the northwest prevail, bringing dry and arid conditions to the region. In contrast, during the monsoon season, the prevailing winds shift to the southwest, bringing moisture-laden air from the Bay of Bengal, resulting in heavy rainfall. During the winter season, the winds are relatively calm, with occasional gusts from the northeast.

Climate Variability

The climate of Nirmali is subject to natural variability and is influenced by larger climate patterns such as the Indian Ocean Dipole (IOD) and the El Niño Southern Oscillation (ENSO). These climate phenomena can lead to fluctuations in rainfall patterns and temperature anomalies, impacting the local climate of Nirmali. Monitoring and understanding these large-scale climate patterns are essential for predicting and managing potential climate-related risks in the region.

Conclusion

Nirmali experiences a subtropical climate with hot summers, cool winters, and a significant amount of rainfall during the monsoon season. The temperature variations and the impact of monsoon showers play a vital role in shaping the region's agricultural productivity and overall climate. Understanding the climate patterns in Nirmali is crucial for various sectors, including agriculture, infrastructure planning, and disaster management. By considering these climatic factors, stakeholders can make informed decisions and develop strategies to mitigate potential risks associated with extreme weather events in Nirmali. Note: The data provided in this article is based on historical weather patterns and may vary from year to year.