A thermocline is a transition layer between warmer water at the surface of a body of water and the cooler deep water that lies below. It is caused by the effect of the sun on the water, in that it keeps the upper parts of the body of water warm whilst being unable to reach the lower, deeper parts.
Correct option is B)
Clearly, from graph the curve increases from x=40 to x=50 and then it start decreasing from x=50 to x=60.
Hence, option B is correct.
Answer:
The correct response is "Cloud seeding".
Explanation:
- A strategy to stimulate as well as enhance the amount of rainfall by spreading dryness ice, as well as iodide particulate matter across storm cloud development throughout a particular location, could be considered as Cloud seeding.
- Dried ice solidifies freshwater raindrops throughout the sky and turns the latter into some raindrop
State some of the land forms of the Morteratsch Glacier.
Answer: U-Shaped Valleys, Fjords, and Hanging Valleys
Glaciers carve a set of distinctive, steep-walled, flat-bottomed valleys. U-shaped valleys, fjords, and hanging valleys are examples of the kinds of valleys glaciers can erode.
Paragraph: It is just after the Pasterze Glacier and Gepatschferner, the third largest and by volume (1.2 km3) the most massive glacier in the eastern alps. The Morteratsch Glacier is a typical valley glacier with a pronounced ice front. The accumulation zone lies between the peaks of Piz Morteratsch, Piz Bernina, Crast' Agüzza, Piz Argient, Piz Zupò and Bellavista. From Piz Argient to the ice front in the Val Morteratsch, its horizontal extent is less than ~6 km (3.7 mi), with an altitude difference of up to 2,000 m (6,600 ft).[citation needed].
Together with the Pers Glacier, originating at Piz Palü, which joins the Morteratsch just below the rock formation Isla Persa ("Lost Isle"), as of 1973 it covered an area of about 16 km2 (6.2 sq mi). The volume of the ice is estimated to be about 1.2 km3.[citation needed] The Morteratsch Glacier drains into the Ova da Morteratsch, which eventually flows into the Inn and hence via the Danube into the Black Sea.[1]
In spring, depending on the snow conditions, a 10-km-long ski-run accessible to skilled skiers is marked on the glacier. It leads from the Diavolezza aerial tramway terminus to the Morteratsch inn and has an altitude difference of 1,100 m (3,600 ft). The Morteratsch railway station used to be situated directly at the ice front of the glacier. The ice front has receded over 2,800 m (9,200 ft) in the meantime (as of 2016), and can no longer be seen from the station.[1][2]
Yearly length change measurements have been recorded since 1878. For the period to 1998, the overall retreat was over 1.8 km (1.1 mi) with a mean annual retreat rate of approximately 17.2 m (56 ft) per year. This long-term average has markedly increased in recent years, receding 30 m (98 ft) per year from 1999–2005. Substantial retreat was ongoing through 2006 as well.[3] During the last ten years, it lost another 1 kilometre (0.62 mi).[4]
Explanation:
During the ending of the glaciation period , the latitudinal climatic belts had developed well and climate was getting warmer. But at the end, there was extreme hot and dry condition that was a threat to marine and land based life. But the best thing was that there evolved diversity in terrestrial life and Pangea had lots of variety of species on it.
But we can not consider it similar to the present day climate since the present day climate change is occurring more because of human activities and is not natural. The climate change in that period was due to internal and external natural factors on the earth since human had not evolved that time to disturb the nature.
