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It is clear that Churchill took his inspiration from various sources, including Hall and Shakespeare.

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Duff Cooper had also given a speech immediately before Churchill's which captured the essence of 'the few and the many', though not as eloquently. Some historians take the view that Churchill was not referring to just the fighter pilots but that his remarks were intended to refer to all allied aircrew, specifically including Bomber Command.

A version of the title of the speech appears in Benjamin Clementine 's song "Winston Churchill's Boy". From Wikipedia, the free encyclopedia. This section needs additional citations for verification.

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Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. Wright M. Halfway to Heaven: Concluding memoirs of a literary life. Stroud Gloucestershire: Sutton.

Descripción de So Much Time, So Little Change Audiobook by Thomas M. Sullivan

Retrieved 1 March The Few. Winston Churchill. Winston Churchill as writer. Hidden categories: EngvarB from September Use dmy dates from September Articles needing additional references from August All articles needing additional references.

It's normal for there to be some greenhouse gases in our atmosphere. They help keep Earth warm enough to live on. But too many greenhouse gases can cause too much warming. The burning of fossil fuels like coal and oil increase the amount of CO 2 in our air. This happens because the burning process combines carbon with oxygen in the air to make CO 2.

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It's important that we monitor CO 2 levels, because too much CO 2 can cause too much warming on Earth. Over millions of years, Earth's climate has warmed up and cooled down many times. However, today the planet is warming much faster than it has over human history.

Wonka, So Much Time

Global air temperatures near Earth's surface have gone up about 2 degrees Fahrenheit in the last century. In fact, the past five years have been the warmest five years in centuries. One-and-a-half degrees may not seem like much. However, this change can have big impacts on the health of Earth's plants and animals.

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We know what Earth's past climate was like by studying things that have been around for a long time. For example, scientists can study what Earth's climate was like hundreds of years ago by studying the insides of trees that have been alive since then.

But if scientists want to know what Earth's climate was like hundreds of thousands to millions of years ago, they study sediment cores and ice cores. Sediment cores come from the bottoms of lakes or the ocean floor. Ice cores are drilled from deep — sometimes miles — below the surface of the ice in places like Antarctica. A drilled ice core kind of looks like what you get if you plunge a drinking straw into a slushy drink and pull it out with your finger over the end of the straw. The layers in an ice core are frozen solid.

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These layers of ice give clues about every year of Earth's history back to the time the deepest layer was formed. The ice contains bubbles of the air from each year. Scientists analyze the bubbles in each layer to see how much CO 2 they contain. Each layer in an ice core tells scientists something about Earth's past. Scientists can also use ice cores to learn about the temperatures for each year.

As snow accumulates onto a growing glacier, the temperature of the air imprints onto the water molecules in the ice. Scientists who use trees, ice cores, and lake and ocean sediment to study Earth's climate are called paleoclimatologists. They look at all of these sources of information and compare their findings to see if they match up. If they do, then their findings are accepted as being most likely true.