Why the climate of Greenland is different than India list any two factors
Answers
Answer:
Greenland has an Arctic climate with average temperatures that do not exceed 10° C (50° F) in the warmest summer months. The air quality in Greenland is among the best in the world due to the country’s geographical position to the high north.
In the southern part of the country and the innermost parts of the long fjords, the temperature can, however, rise to more than 20° C (68° F) in June, July or August, and due to the fine air quality and low levels of moisture in the air, in general you are able to see very, very far.
VARIABLE COASTAL AND INLAND CLIMATE
The sea around Greenland affects the climate on land. The stretches of coastline close to the open sea, in particular, are cooled by the sea.
Therefore during the summer months it is warmest and driest on land closest to the ice sheet. In all parts of the country the weather is locally changeable and can vary from fjord to fjord and from one valley to the next.
You can get the best weather information by enquiring at local tourist offices or asking local people.
LOW HUMIDITY
The air is generally very dry in Greenland in relation to many other countries, and because of this low humidity the low temperatures do not feel as cold as you might expect. On the other hand, the dry air means that you must drink more water than normal.
The low humidity also means that you can see further than you are probably used to. Mountain crests that appear to be close are usually further away than you think so keep this in mind when planning a hike.
The climate of India comprises a wide range of weather conditions across a vast geographic scale and varied topography, making generalisations difficult. Based on the Köppen system, India hosts six major climatic subtypes, ranging from arid deserts in the west, alpine tundra and glaciers in the north, and humid tropical regions supporting rainforests in the southwest and the island territories. Many regions have starkly different microclimates, making it one of the most climatically diverse countries in the world. The country's meteorological department follows the international standard of four climatological seasons with some local adjustments: winter (December, January and February), summer (March, April and May), a monsoon means rainy season (June to September), and a post-monsoon period (October to November).
In INDIA geography and geology are climatically pivotal: the Thar Desert in the northwest and the Himalayas in the north work in tandem to effect a culturally and economically important monsoonal regime. As Earth's highest and most massive mountain range, the Himalayas bar the influx of frigid katabatic winds from the icy Tibetan Plateau and northerly Central Asia. Most of North India is thus kept warm or is only mildly chilly or cold during winter; the same thermal dam keeps most regions in India hot in summer.
Though the Tropic of Cancer—the boundary between the tropics and subtropics—passes through the middle of India, the bulk of the country can be regarded as climatically tropical. As in much of the tropics, monsoonal and other weather patterns in India can be wildly unstable: epochal droughts, floods, cyclones, and other natural disasters are sporadic, but have displaced or ended millions of human lives. There is one scientific opinion which states that in South Asia such climatic events are likely to change in unpredictability, frequency, and severity. Ongoing and future vegetative changes and current sea level rises and the attendant inundation of India's low-lying coastal areas are other impacts, current or predicted, that are attributable to global warming.
