Climate Change Essays

Climate Change Essays-12
The IPCC has projected that global average surface temperatures could increase 1.4 to, 5.8°C by 2100.

The IPCC has projected that global average surface temperatures could increase 1.4 to, 5.8°C by 2100.Daily maximum and minimum temperatures will increase as well as the number of hot days-, with less cold and frosty days.

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Reliable temperature records began in 1850 and our world is now about one degree Celcius hotter than it was in the period between 18 – commonly referred to as the "pre-industrial" average.

The change is even more visible over a shorter time period – compared to average temperatures between 19, 2017 was 0.68 degrees warmer, while 2016 was 0.8 degrees warmer, thanks to an extra boost from the naturally-occurring El Niño weather system.

The Intergovernmental Panel on Climate Change (IPCC) reported that the Earth’s average surface temperature during the 20th century increased approximately 0.6°C.

While this may seem like a small change, global temperatures are generally quite stable.

While this temperature increase is more specifically referred to as global warming, climate change is the term currently favoured by science communicators, as it explicitly includes not only Earth's increasing global average temperature, but also the climate effects caused by this increase.

Attention has begun to shift from local, short-term seasonal patterns of temperature, rainfall, other elements of the weather, toward longer-term trends that can affect the entire Earth, se long-term (typically 30-year) weather trends are called “climate.” It is therefore important understand the difference, as well as the relation, between “weather” and “climate.” An example of the relationship between weather and climate is El Nino, which is weather with local, short-term consequences as well as with global, long-term importance. El Nino can bring a dry summer for some regions and a wet winter for others; however, over the course of many years, the number of times El Nino conditions occur may decade changes in the global climate.

Variations in the behaviour of the weather over long time periods, such as from one century another, are referred to as climate change.

Climate itself adjusts from the times of ‘ice ages,’ hen huge ice sheets covered large areas that are currently ice-free, to periods similar to today hen ice sheets are largely confined to Antarctica, Greenland, and the floating Arctic sea ice.

In that case, we talk of a change in climate or climatic change.

Various terms used to describe variations in climate, namely, climate variability.


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