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Siberian High

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January 10, 2026

Prelims: Current events of national and international importance | Geography

Why in News?

The Siberian High has recently drawn attention due to its strong winter activity, influencing cold weather conditions across parts of Asia, including India.

  • Siberian High It is an intense, robust system of cold, dry air and high atmospheric pressure that controls winter weather across Eurasia.
  • Location Centered near Lake Baikal in Siberia, it's also known as the Asiatic High or Siberian anticyclone.
  • Intensity It is the strongest semi-permanent high-pressure system in the Northern Hemisphere, with pressure often exceeding 1040 millibars.
  • Vertical Extent - It is a shallow system, rarely persisting above altitudes of 3,000 meters (10,000 feet).
  • Nature of Air It is extremely cold and dry air.
  • Formation Radiative Cooling - The high forms due to intense cooling of the Earth's surface over the vast Asian landmass.
  • During the long winter nights, heat escapes into space, causing the air near the surface to become dense, heavy, and cold.
  • Winter Peak - It reaches its maximum strength in midwinter (January/February) and drives the northeast monsoon in East and South Asia.
  • Summer Dissipation- In the summer months, the system is replaced by the Asiatic Low, which brings the summer monsoon.
  • Climatic Drivers of Variability - Arctic Oscillation (AO) – Arctic Oscillation (AO) / North Atlantic Oscillation (NAO)
    • Negative AO stronger Siberian High.
    • Positive AO weaker high.
  • ENSO (El Niño–Southern Oscillation)
    • El Niño years may weaken the Siberian High; La Niña can strengthen it (not always consistent).
  • Eurasian Snow Cover - Greater autumn snow cover stronger winter Siberian High.
  • Climate Change - Arctic amplification may reduce temperature gradients, potentially weakening the Siberian High, though episodic extreme cold events may persist.
  • Impact on India Siberian High drives cold northerly winds towards India.
  • It is a key reason for cool winters in North India.
  • The Himalayas generally block the most extreme cold associated with the Siberian High.
  • During La Niña conditions, the Siberian High can overcome the Himalayan barrier and move southward.

Reference

The Hindu | Siberian High

 

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