An Unbiased View of Selected Water Resources Abstracts

The primary streams draining the northern part of the county consist of Dickey Brook, Furnace Brook, Hallocks Mill Brook, Hunter Brook, Muscoot River, Peekskill Hollow Brook, and Titicus River. The county consists of several significant reservoirs; The Croton system and the Kensico Tank are essential parts of the New york city City water supply system.

The elements of the system consist of the New Croton Reservoir, the Cross River Tank, the Titicus Tank, the Amawalk Reservoir, and the Muscoot Tank. Other significant reservoirs are the Kensico and Byram Lake Tank, while there are a variety of smaller tanks throughout the county. The Westchester County Department of Preparation divides the county into North, Central and South sub-regions.

Environment [modify] The environment of Westchester County is primarily a damp subtropical environment (Koppen Cfa), with higher elevations bordering on a humid continental environment. Keep Checking Back Here are cold, wet, and periodically snowy throughout the county, with more snow inland in higher elevations. Summer seasons are hot inland but cooler towards the coast, with rather of a relative dryness in the early part of summer season.

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Snowfall is more typical in Westchester than in New York City City, with the exception of the southeast of the county where snowfall is often between 20 and 25 inches. In January, inland areas have a low of 2126 F and a high of 3437 F while seaside locations have a low of 2730 F and a high of 3841 F.

Coastal areas, consisting of Mamaroneck, New Rochelle, Rye, and Port Chester have highs of 8183 F and lows of 6873 F, while inland highs will be 8487 F and lows will be 6570 F. Winds can be heavy, especially by the coast. Demographics [edit] Historical population Census Pop. % 23,97827,42814. 4%30,27210. 4%32,6387.