Current Affairs 25th March 2025
Current affairs 25th March 2025 by Saurabh Pandey Sir
Judicial Transfers in India Key Aspects of Judicial Transfers
⚖ Transfer Procedure: Judges are transferred after consultation with the Chief Justice of India.
Presidential Authority: The President has the authority to transfer judges between courts.
📜 Article 222: This article provides provisions for transferring judges from one high court to another.
Chief Justice’s Role: The Chief Justice of India plays a crucial role in the decisionmaking process for judge transfers.
📚 Historical Context: There have been various cases of judge transfers in Indian constitutional history.
Federation Concepts: The transfer of high court judges is influenced by the concepts of “Quasi Federation” and “Cooperative Federation.”
🏛 Guidance of Article 222: The transfer process is guided by Article 222 of the Indian Constitution. Boreal Summer Intraseasonal Oscillation (BSISO), and Indian Monsoon
● An IISc release said that India receives 80% of its annual rainfall during the summer monsoon between June and September, which are marked by several wet and dry spells along with strong winds.
● These spells are controlled by the Boreal Summer Intraseasonal Oscillation (BSISO), also called monsoon intraseasonal oscillations, which also brings a cloud band from the equator over to the Indian subcontinent, putting an end to the dry spell.
● The duration of the wet spell is determined by the size and strength of the cloud band. “Most of the existing literature says that even if you put any small instability, it should always propagate northwards. What we have shown is that this is not the case. If the cloud band in The equator is weak to start with, then it cannot propagate north,
The boreal summer intraseasonal oscillation (BSISO) is among the most pronounced subseasonal variability in the tropics during the boreal summer. Compared with its wintertime counterpart, the so-called Madden–Julian oscillation (MJO), the BSISO convection displays more complicated spatiotemporal evolution, characterized by northward propagation over the northern Indian Ocean and western North Pacific as well as eastward propagation along the equator. It exerts a strong effect on a broad range of tropical weather and climate phenomena, such as tropical cyclogenesis, monsoon onset, and active/break cycles, among others. Spatiotemporal Dynamics of BSISO The BSISO’s spatiotemporal dynamics are fascinating and crucial for understanding its impact on tropical weather systems. Propagation Patterns: The BSISO typically exhibits a northward movement across the northern Indian Ocean and western North Pacific.
