The Reason England is Subject to Unpredictable Weather, the Reason England is Subject to Frequent and Drastic Changes Within Weather, the Altitude at Which Most Weather Occurs, the Reason Weather Within the Stratosphere is More Stable Than Weather Within the Troposphere, the Location of the Tropospheric Jet Stream Within the Atmosphere, the Concept of the “Quasi-Biennial Oscillation”, the Impact of Quasi-Biennial Oscillation Within the Northern Hemisphere, the Equatorial Wind Direction Which Strengthens the Tropospheric Jet Stream, How the Earth’s Temperature Affects the Tropospheric Jet Stream, the Correlation Between the Earth’s Temperature and the Intensity of Rain, the Analog of the Tropospheric Jet Stream, the Concept of a “Meander” Within a River, the Reason Rivers Slow Down, the Correlation Between River Gradient and Tropospheric Jet Stream Temperature, the Rate the Arctic is Melting During the Modern Day and the Concept of “Arctic Amplification”, the Volume of Summer Sea Ice Which Has Disappeared Post 1984, the Density of Sea Ice During the Modern Day vs the Density of Sea Ice During the Mid 20th Century, and the Reason Melting Sea Ice Impacts Climate Change and the Earth’s Oceans

The UK is subject to such unpredictable weather because to the north it must contend with the arctic air mass bringing cold snowy weather, to the east comes the polar continental air mass dragging bitter winds in from Siberia, to the south floods in the tropical air mass bringing warm air up from North Africa, and to the west brings the maritime air mass with mild wet weather from the Atlantic. None of these air masses dominate which leaves the UK subject to frequent and drastic changes in weath...


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