Main Body
of Indian Soumni branch come about Indian subcontinentBrahki 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 downwardsbreak in NE India,
b upwardsmore rainfall in Northern plains.
4Monsoon Distribution
cause more rainfall during monsoons.
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
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