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Current region 212: 1947 New York City: Manhattan only; overlays with 332, 646, and 917 315: 1947 Syracuse, Utica, Watertown, and north central New York; overlaid by 680. 329: 2023: Poughkeepsie, Middletown, Newburgh, West Point, Goshen and southeastern New York; overlay of 845 332: 2017: New York City: Manhattan only; overlays with 212, 646 ...
The annual average temperature across the state ranges from around 39 °F (4 °C) over the Adirondack Mountains to near 53 °F (12 °C) across the Hudson Valley and Long Island, to around 56 °F (13 °C) within New York City. [2] Weather in New York is heavily influenced by two air masses: a warm, humid one from the southwest and a cold, dry ...
Geographic limits of the map:}} *N: 45.30° N *S: 40.30° N *W: 80.20° W *E: 71.00° W Albers equal area projection; WGS 84 datum |date=2019-09-21 |source={{own}} *Sources of data:<br/> **Topography: ETOPO1 (public domain);<br/> **Public domain data provided by the National Atlas of the United States of America;<br/> *Tool:<br/> **The map is ...
If this map is the primary area code map of New York (master map), no area code appears in red. Map is correct as of January 2, 2013. All New York telephone Area Code maps are now using the SVG file format due to the regular need for changes, the older PNG image format maps have been deprecated and will no longer be maintained, changed ...
Schematic of the Birkeland or Field-Aligned Currents and the ionospheric current systems they connect to, Pedersen and Hall currents. [1]A Birkeland current (also known as field-aligned current, FAC) is a set of electrical currents that flow along geomagnetic field lines connecting the Earth's magnetosphere to the Earth's high latitude ionosphere.
New York City can occasionally experience strong winds, like many coastal locations. Tropical cyclones or intense oceanic storms bring the strongest winds. The strongest gust in Central Park, of 78 miles per hour (126 km/h), occurred on December 2, 1974, however, a station at The Battery reported a gust of 113 miles per hour (182 km/h) on ...
The worldwide solar-driven wind results in the so-called Sq (solar quiet) current system in the E region of the Earth's ionosphere (ionospheric dynamo region) (100–130 km (60–80 mi) altitude). [citation needed] Resulting from this current is an electrostatic field directed west–east (dawn–dusk) in the equatorial day side of the ionosphere.
The plasmasphere, or inner magnetosphere, is a region of the Earth's magnetosphere consisting of low-energy (cool) plasma. It is located above the ionosphere . The outer boundary of the plasmasphere is known as the plasmapause , which is defined by an order of magnitude drop in plasma density.