Sweden
Geography
However, Sweden is much warmer and drier than other places at a similar latitude, and even somewhat farther south, mainly because of the combination of the Gulf Stream and the general west wind drift, caused by the direction of planet Earth's rotation. Continental west-coasts (to which all of Scandinavia belongs, as the westernmost part of the Eurasian continent), are notably warmer than continental east-coasts; this can also be seen by comparing e.g. the Canadian cities of Vancouver and Halifax, Nova Scotia with each other, the winter in west coast Vancouver is much milder; also, for example, central and southern Sweden has much milder winters than many parts of Russia, Canada, and the northern United States. Because of Sweden's high latitude, the length of daylight varies greatly. North of the Arctic Circle, the sun never sets for part of each summer, and it never rises for part of each winter. In the capital, Stockholm, daylight lasts for more than 18 hours in late June but only around 6 hours in late December. Sweden receives between 1,100 and 1,900 hours of sunshine annually. During July there is not much difference in temperature between the north and south of the country. With the exception of in the mountains, the whole country has a July-average temperature within the range of 15 °C (59 °F) to 17.5 °C (63.5 °F) (a difference of 2.5 degrees Celsius), while the January-average temperatures vary from freezing point down to below −15 °C (5 °F) along the border with Finland (a difference of 15 degrees Celsius)
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