Question

Give a geographical reason for each of the following:
1. Kanpur has extreme temperature conditions.
2. Kochi is warmer than Mumbai even though they both lie on the Western coast of India.
3. The Ganga Plain gets the monsoon rain much later than the west Coast of India.

Answer 1

Hint: Geography is frequently demarcated in terms of 2 branches: human geography and physical geography. Human geography is related to the analysis of people and their societies, beliefs, economies, and communications with the environment by reviewing their interactions with and across space and place. Physical geography is related with the analysis of procedures and precedents in the natural environment like the atmosphere, hydrosphere, biosphere, and geosphere.

Complete answer:
The environment of Uttar Pradesh (U.P.) is mostly distinct as moist subtropical with dry winter type with fragments of Western U.P. as a semi-arid type. Otherwise, some authors denote it as a tropical monsoon. Differences do happen in dissimilar portions of the large state, nevertheless the consistency of the massive Indo-Gangetic Plain creating majority of the state gives a principally solitary climatic precedent to the state with slight regional differences. U.P. has an environment of extravagances. With temperatures inconsistent wherever from 0 °C to 50 °C in numerous parts of the state and recurring droughts and inundations owing to random rains, the summers are tremendously hot, winters cold and rainy season can be either extremely wet or extremely dry.
Kochi is warmer than Mumbai although they both lie on the western coast of India as the prior is situated adjacent to the Equator and collects direct emissions of the Sun all through the year.
The 2nd division of the Arabian Sea assaults the western coast of India by the 2nd week of June. The Ganga Plains collect precipitation from the Bay of Bengal division which initially assaults the north-eastern portions of India and afterward journeys to the Northern Ganga Plains.

Note: The Himalayas operate as a barricade to the frosty katabatic winds emanating down from Central Asia. Therefore, northern India is kept warm or just slightly cooled throughout winter; in summer, the similar occurrence makes India comparatively hot.