Main Body
of Indian Soumni branch come about Indian subcontinent → Brahki monsoon.
2Somali jet stream & Tibetan clearly Jet stream
Tibetan (Tibetan clearly (LP Distension) TESS
Convergent stream
Orassanthus (LH)
Somali jet stream 1 TESS drains more rainfall.
3Fluctuation of ITCZ
6 downwards → break in NE India,
b upwards → more rainfall in Northern plains.
4Monsoon Distribution
cause more rainfall during monsoons.
— Abhimanyu Malik · AIR 60
66 words8 paragraphs
Diagram
Map of India showing Tibetan stream, TESS, convergent stream, and Orassanthus (LH) systems with arrows indicating directional flow
- Identified multiple atmospheric circulation patterns (Somali jet stream, Tibetan jet stream)
- Connected ITCZ fluctuation to monsoon behavior
- Provided geographic specificity (NE India, Northern plains)
- Explained monsoon distribution mechanisms
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Topper
Abhimanyu Malik
AIR 602023
Subject & Paper
GS1GS1
Topic
Indian Geography
River Systems
Himalayan Rivers and Tributaries
Writing Stats
66
Total words
8
Paragraphs
Technical and structured
Tone