Climate of Delaware
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Delaware, primarily situated within the Atlantic Coastal Plain, ranks second only to Florida for its low average elevation. Its oceanfront features a lengthy stretch of sandy beach, extending from Fenwick Island, at the Maryland border, to Cape Henlopen, at the mouth of Delaware Bay. Along its 23-mile (37-km) length, only one major break, Indian River Inlet, interrupts the coastline. The beach mostly consists of a low bar nestled between the ocean and a series of lagoons or shallow bays. However, at Bethany Beach, near the southern boundary, and again at Rehoboth Beach, near the northern end, the mainland extends directly to the ocean.
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A significant portion of Delaware Bay's shoreline consists of marshland. The mouths of tributaries like the Murderkill, the Mispillion, and the St. Jones are shallow, offering safe harbors primarily for fishing boats north of Lewes. Moving northward along the banks of the Delaware River, elevated and dry areas emerge, notable at locations such as Port Penn, New Castle, and Edgemoor. Wilmington, the state's primary port, sits at the junction of the Delaware River and the Christina River, one of its tributaries.
Most of Delaware's drainage is directed eastward toward the Delaware River, Delaware Bay, and the Atlantic Ocean. However, the Nanticoke River and its tributaries in the southwestern part of the state flow into Chesapeake Bay. Similarly, the Pocomoke River, draining the Cypress Swamp or "Burnt Swamp" in the extreme south of Delaware along the Maryland border, also empties into Chesapeake Bay.
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The Coastal Plain of Delaware is predominantly fertile and flat, rarely reaching heights above 60 feet (18 meters) above sea level. However, as one moves southward, it gradually becomes sandier. Near its northern boundary, the plain is traversed by the Chesapeake and Delaware Canal, which has been widened and straightened to accommodate ocean shipping. This canal significantly reduces the water route between Philadelphia and Baltimore, Maryland, by several hundred miles, effectively bringing Baltimore closer to the ocean compared to the route via Chesapeake Bay. Popularly viewed as the dividing line between the agricultural southern region and the industrial north, the canal is believed by many Delawareans to mark a change in weather patterns as well.
Key landmarks visible from afar include several elevated bridges spanning the canal, the imposing twin bridges over the Delaware River north of New Castle, and the prominent refinery stacks in Delaware City. These landmarks stand against the backdrop of the rolling hills of the Piedmont, extending south from Pennsylvania into the northwestern corner of the state. Until the mid-20th century, the landscape south of Wilmington was characterized by farmlands, forests, streams, and ponds, dotted with occasional villages. However, suburban development has since expanded to encompass areas flanking the canal, encroaching upon the remaining farmlands in New Castle County.
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The highest elevation in Delaware, situated just off Ebright Road in New Castle County near the Pennsylvania border, reaches a modest 448 feet (137 meters) above sea level. Notable geographical features include Iron and Chestnut hills, located southwest of Newark, characterized by exposed pits from historic iron ore mining activities.
Wilmington's city center is positioned atop hills that slope downward toward the meeting point of the Christina River and its primary tributary, the Brandywine. This strategic location offered navigable waters close to waterfalls, which historically provided power for manufacturing industries. The presence of railroads and highways, tracing the fall line along the East Coast, has positioned Wilmington along major transportation arteries connecting Philadelphia and Baltimore. See more: https://weatherusa.app/zip-code/weather-19736 This geographic advantage has fueled urbanization trends, fostering development in the open spaces between Wilmington and neighboring cities.
Delaware's climate is characterized as humid and temperate. At New Castle Airport in northern Delaware, the average daily temperature hovers around 54°F (12°C), with July typically recording the highest average high temperatures at 86°F (30°C), and January registering the lowest average lows at 23°F (−5°C). Temperatures tend to be slightly warmer in southern Delaware, generally running about two degrees higher than those recorded in the north. August, ranking as the second warmest month after July, also stands out as the rainiest, with an average precipitation of approximately 5.5 inches (140 mm). Conversely, February sees the least amount of precipitation, averaging about 3 inches (75 mm). Annually, Delaware receives an average precipitation of nearly 45 inches (1,140 mm).
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