North Carolina
Due to its wide range of elevation, from sea level on the coast to over 6,000 feet in the mountains, North Carolina has the most variation in climate of all the Southeastern states. The climate in the coastal and Piedmont regions of eastern and central North Carolina is similar to other Southern states such as Georgia or South Carolina, while the climate in the western mountains is closer to that found in New England or the upper Midwest. While the coastal plains, especially the tidewater areas, are strongly influenced by the Atlantic Ocean, the western, mountainous part of the state is more than 300 miles from the coast, and there is considerably less maritime influence there. As such, the climate of the state ranges from a warm, humid subtropical climate near the coast to one which is humid climate in the mountains. Most of the state falls in the humid subtropical zone.
North Carolina is bordered by South Carolina on the south; Georgia on the southwest; Tennessee on the west; Virginia on the north; and the Atlantic Ocean on the east. The United States Census Bureau classifies North Carolina as a Southern state in the subcategory of being one of the South Atlantic States.
North Carolina consists of three main geographic sections: the coastal plain, which occupies the eastern 45% of the state; the Piedmont region, which contains the middle 35%; and the Appalachian Mountains and foothills, which take up the remaining 20% of the state in the west. The coastal plain begins in the east as a chain of narrow, sandy barrier islands known as the "Outer Banks". The Outer Banks encompass two sounds — Albemarle Sound in the north and Pamlico Sound in the south; they are the two largest landlocked sounds in the United States. Inland the coastal plain is relatively flat, with rich soils which grow tobacco, soybeans, and cotton. The major rivers of this section, the Neuse River, Tar River, Pamlico River, Cape Fear River, and Roanoke River, tend to be slow-moving and wide.
The coastal plain turns into the Piedmont region along the "fall line", a line which marks the elevation at which waterfalls first appear on streams and rivers. The Piedmont region of central North Carolina is the state's most urbanized and densely-populated section - all five of the state's largest cities are located in the Piedmont. It consists of gently rolling countryside frequently broken by hills or low isolated mountain ridges. Many small, deeply eroded mountain ranges and peaks are located in the Piedmont, including the Saura Mountains, Pilot Mountain, the Uwharrie Mountains, Crowder's Mountain, King's Pinnacle, the Brushy Mountains, and the South Mountains. The Piedmont ranges from about 300–400 feet (90–120 m) elevation in the east to over 1,000 feet (300 m) in the west. The major rivers of the Piedmont, such as the Yadkin and Catawba, tend to be fast-flowing, shallow, and narrow.
The western section of the North Carolina is part of the Appalachian Mountain range. Among the subranges of the Appalachians located in the state are the Great Smoky Mountains, Blue Ridge Mountains, Balsams, Pisgahs, and the Black Mountains. The Black Mountains are the highest mountains in the Eastern United States, and culminate in Mount Mitchell at 6,684 feet (2,037 m). It is the highest point east of the Mississippi River. Due to the higher altitude in the mountains, the climate often differs starkly from the rest of the state. Winters in western North Carolina typically feature significant snowfall and subfreezing temperatures more akin to a northern state than a southern one.
The three geographical divisions of North Carolina are useful when discussing the climate of the state. The coastal plain is influenced by the Atlantic Ocean and helps keep the temperatures down in the summer and up in the winter. Daytime high temperatures on the coast average less than 90oF during the summer. In the winter, the coast has the mildest temperatures in the state. The coast typically has around one or two winter storms (snow/ice) every year and receives around 1 inch of snow annually. The Piedmont has hotter summers with daytime highs averaging over 90oF in many locations. While it is not common for temperatures to reach over 100oF in North Carolina, when it happens, the highest temperatures are to be found in the lower areas of the Piedmont, especially around the city of Fayetteville. In the winter, the Piedmont is much less mild than the coast, with temperatures that can reach 20oF or below, and around 8–10 inches of annual snowfall. Annual precipitation and humidity is lower in the Piedmont than either the mountains or the coast, but even at its lowest, the precipitation is a generous 40 inches a year. The Appalachian Mountains are the coolest area of the state, with temperatures frequently falling into the teens or lower in the winter, and relatively cool summers which rarely rise above 80oF. Snowfall in the mountains is usually 14–20 inches per year, but can be much higher in the higher elevations.
Severe weather is not a rare event in North Carolina. On average, the state receives a direct hit from a hurricane once a decade, although in some years several hurricanes or tropical storms can either directly hit the state, or brush across the coastal areas. Only Florida and Louisiana are hit by the storms more often. On average, North Carolina has 50 days of thunderstorm activity per year, with some storms becoming severe enough to produce hail and strong, damaging winds. North Carolina averages less than 20 tornadoes per year, and some of these are produced by hurricanes or tropical storms along the coast. Nonetheless, tornadoes from thunderstorms are a risk, especially in the Piedmont region of central North Carolina.
According to the U.S. Census Bureau, as of 2005, North Carolina has an estimated population of 8,683,242, which is an increase of 142,774, or 1.7%, from the prior year and an increase of 636,751, or 7.9%, since the year 2000. This exceeds the rate of growth for the United States as a whole. The growth comprises a natural increase since the last census of 248,097 people (that is 627,309 births minus 379,212 deaths) and an increase due to net migration of 390,672 people into the state. Immigration from outside the United States resulted in a net increase of 158,224 people, and migration within the country produced a net increase of 232,448 people. North Carolina has historically been a rural state, with most of the population living on farms and in small towns. However, over the last 25 years the state has undergone rapid urbanization, and today the residents of North Carolina live primarily in urban areas, as is the case in most of the United States. In particular, the cities of Charlotte and Raleigh have become major urban centers, with a large, diverse, and rapidly-growing population. Most of this growth in diversity has been fueled by immigrants from Latin America, especially Mexico. The state has also witnessed a large increase in the number of immigrants from Asia, especially India and countries in Southeast Asia, such as Vietnam.