Explanation:

Concordant Drainage- Peninsular India
Antecedent drainage- Himalayan region
Jet Stream- Upper atmospheric zone
Inland drainage- Desert area

A part of a river slope and the surrounding area gets uplifted and the river sticks to its original slope, cutting through the uplifted portion like a saw [Vertical erosion or Vertical down cutting], and forming deep gorges: this type of drainage is called Antecedent drainage.

A drainage pattern is described as concordant if it correlates to the topology and geology of the area. In simple words: In a concordant drainage pattern, the path of the river is highly dependent on the slope of the river and topography.

Inland drainage is that drainage in which rivers do not reach an ocean or sea but empty their waters in a lake or an inland sea. Main Characteristics of Inland Drainage: i. In inland drainage streams join lakes or inland seas.

Jet streams are fast moving, permanently oriented upper atmospheric circulations that circumnavigate the earth