Geography & Climate of Saharanpur

Saharanpur is located in the northernmost part of the Ganga–Yamuna Doab, at the foothills of the Shivalik range. The district occupies a strategically important position, forming a transition zone between the Himalayan foothills and the Upper Gangetic Plains.

Boundaries

• North: Dehradun District (Uttarakhand)

• East: Haridwar District (Uttarakhand)

• West: Yamuna River (boundary with Haryana)

• South: Muzaffarnagar District (Uttar Pradesh)

Latitudinal & Longitudinal Extent

• Latitude: 29°34′45″ N to 30°21′30″ N

• Longitude: 77°09′00″ E to 78°14′45″ E

The district covers an area of approximately 3,860 square kilometres and became a separate administrative division in 1997.

Physiographic Regions

The physical landscape of Saharanpur is distinct from much of western Uttar Pradesh and can be broadly divided into four natural regions:

1. Shivalik Hill Tract – The northernmost belt, characterised by low hills, forests, and seasonal streams.

2. Bhabar Region – A porous belt at the foothills, composed of coarse sediments where rivers often disappear underground.

3. Bangar Region – The elevated alluvial plain, forming the main habitable and cultivated area.

4. Khadar Region – The low-lying floodplain along rivers, especially the Yamuna, consisting of fertile alluvial soil.

Rivers & Drainage

The Yamuna River is the principal river of the district, forming its western boundary. Several seasonal and perennial tributaries, including the Solani, Hindon, Ratmau, Nagdev, Paondhoi, and Dhamola, traverse the district and play a vital role in drainage, soil formation, and groundwater recharge.

Climate

Saharanpur experiences a sub-humid tropical climate, influenced by its proximity to the Himalayan foothills. Summers extend from March to June, while winters last from October to February, with January being the coldest month.

During the summer season, temperatures generally range between 30°C and 42°C, and may occasionally rise up to 45°C. In winter, temperatures typically vary from 5°C to 20°C, with minimum temperatures sometimes dropping to around 3°C.

The district receives an average annual rainfall of approximately 900 mm to 1,100 mm, most of which occurs during the south-west monsoon (June to September). The intensity and distribution of monsoon rainfall have a direct impact on agricultural activities in the region.

Humidity levels are generally higher during and after the monsoon season, particularly in the northern and western parts of the district. During winter, occasional rainfall due to western disturbances is observed, which is beneficial for rabi crops.

Fog is a common phenomenon in winter, especially during December and January, often affecting visibility.