UPSC MainsGEOGRAPHY-PAPER-II201420 Marks
Q7.

Describe the salient climatological characteristics of Rayalaseema region.

How to Approach

This question requires a detailed understanding of the climatic conditions prevalent in the Rayalaseema region of Andhra Pradesh. The answer should focus on temperature, rainfall, humidity, and other relevant climatological factors. A regional context, highlighting the influence of geographical features and monsoon patterns, is crucial. Structure the answer by first introducing the region, then detailing its temperature regime, rainfall patterns, humidity, and finally, any specific climatic features like droughts or cyclonic influences.

Model Answer

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Introduction

Rayalaseema, meaning ‘stone land’, is a dry and semi-arid region in Andhra Pradesh, comprising eight districts – Anantapur, Chittoor, Kurnool, YSR Kadapa, and parts of Nellore and Prakasam. Geographically, it lies south of the Nallamala Hills and is characterized by undulating terrain and a rain shadow effect. This region experiences a unique climate significantly different from the coastal Andhra region, making it prone to droughts and water scarcity. Understanding its climatological characteristics is vital for effective water resource management and agricultural planning in the region.

Temperature Regime

Rayalaseema experiences extreme temperatures. Summers (March to May) are intensely hot, with average maximum temperatures ranging from 40°C to 45°C, and sometimes exceeding 47°C. The hottest months are May and June. The region experiences a significant diurnal temperature range, meaning a large difference between day and night temperatures. Winters (November to February) are mild and pleasant, with average minimum temperatures ranging from 15°C to 20°C. Frost is occasionally reported in some parts of the region during January.

Rainfall Patterns

The rainfall in Rayalaseema is highly erratic and unreliable. The region receives most of its rainfall from the Southwest Monsoon (June to September) and to a lesser extent from the Northeast Monsoon (October to December). The average annual rainfall varies between 600 mm to 800 mm, significantly lower than the national average. The southwest monsoon is often weak and breaks prematurely due to the rain shadow effect caused by the Western Ghats and the Nallamala Hills. The region is highly susceptible to drought conditions, with frequent failures of the monsoon.

Humidity

Humidity levels in Rayalaseema are generally low, especially during the summer months. The relative humidity during summer often drops below 30%. During the monsoon season, humidity increases to around 70-80%, but it is still lower compared to the coastal regions of Andhra Pradesh. Low humidity contributes to the arid conditions and increases evapotranspiration rates.

Specific Climatic Features

  • Drought Prone Area: Rayalaseema is classified as a chronically drought-prone area. According to the Drought Management Cell, Government of Andhra Pradesh (as of 2022 data), Anantapur and Kurnool districts are consistently identified as the most drought-affected.
  • Cyclonic Influences: While not directly hit by severe cyclones as frequently as the coastal areas, Rayalaseema can experience the effects of cyclones originating in the Bay of Bengal, leading to heavy rainfall and localized flooding.
  • Wind Patterns: The region experiences dry and hot winds during summer, known as ‘loo’. During the monsoon season, the winds are predominantly southwesterly.
  • Soil Erosion: Due to sparse vegetation cover and intense rainfall events (though infrequent), Rayalaseema faces challenges related to soil erosion.

Comparison with Coastal Andhra

Feature Rayalaseema Coastal Andhra
Average Rainfall 600-800 mm 1100-1500 mm
Temperature (Summer Max) 40-47°C 30-35°C
Humidity Low (30-70%) High (70-90%)
Drought Frequency High Moderate

Conclusion

In conclusion, the Rayalaseema region is characterized by a hot and dry climate with erratic rainfall, low humidity, and a high susceptibility to droughts. These climatological characteristics significantly impact the region’s agriculture, water resources, and overall socio-economic development. Sustainable water management practices, drought mitigation strategies, and promoting climate-resilient agriculture are crucial for ensuring the long-term well-being of the region and its population. Further research into micro-climatic variations within Rayalaseema could help tailor interventions for greater effectiveness.

Answer Length

This is a comprehensive model answer for learning purposes and may exceed the word limit. In the exam, always adhere to the prescribed word count.

Additional Resources

Key Definitions

Rain Shadow Effect
The rain shadow effect is a phenomenon where a mountain range blocks prevailing winds, causing one side (windward side) to receive abundant rainfall while the other side (leeward side) remains dry. Rayalaseema experiences this due to the Western Ghats and Nallamala Hills.
Diurnal Temperature Range
The difference between the highest and lowest temperatures recorded during a 24-hour period. Rayalaseema exhibits a large diurnal temperature range, particularly during the summer months.

Key Statistics

Approximately 75% of Rayalaseema’s geographical area is considered drought-prone.

Source: Government of Andhra Pradesh, Drought Management Cell (2022)

The average annual groundwater depletion rate in Rayalaseema is estimated to be around 2-3 meters per year (as of 2020).

Source: Central Ground Water Board (CGWB), Andhra Pradesh (2020)

Examples

Integrated Watershed Management Programme (IWMP)

The IWMP, implemented in Rayalaseema, focuses on holistic watershed development to improve water availability, soil conservation, and livelihood opportunities. It involves community participation and aims to enhance the resilience of the region to drought.

Frequently Asked Questions

Why is Rayalaseema prone to droughts?

Rayalaseema’s location in the rain shadow of the Western Ghats and Nallamala Hills, coupled with the erratic nature of the monsoon, makes it highly susceptible to droughts. The region receives significantly less rainfall compared to other parts of Andhra Pradesh.

Topics Covered

GeographyIndian ClimateRegional GeographyMonsoon