PEQUANNOCK RIVER CONDITIONS
|Pequannock River - Macopin Intake Dam, West Milford, NJ, USGS Current Data at |
Height: feet Flow: ft3/sec Temperature:°C (32°F)
|rt23.com Weather Station|
|Morristown Municipal, NJ, United States (KMMU) 40-48N 074-25W|
|Feb 27, 2017 - 06:45 PM EST / 2017.02.27 2345 UTC|
|Wind: from the WSW (240 degrees) at 5 MPH (4 KT)|
|Visibility: 10 mile(s)|
|Sky conditions: partly cloudy|
|Temperature: 48 F (9 C)|
|Dew Point: 28 F (-2 C)|
|Relative Humidity: 45%|
|Pressure (altimeter): 30.4 in. Hg (1029 hPa)|
|ob: KMMU 272345Z 24004KT 10SM SCT055 09/M02 A3040|
updated: 624 PM EST Mon Feb 27 2017
Mostly cloudy. Lows in the mid 30s. Southwest winds around 5 mph this evening...becoming light and variable.
Partly sunny. A slight chance of light rain in the afternoon. Highs in the upper 50s. Southeast winds around 5 mph. Chance of rain 20 percent.
Rain likely. Areas of fog. Lows around 50. South winds around 5 mph. Chance of rain 60 percent.
Cloudy. Areas of fog in the morning. Light rain likely in the morning...then showers and thunderstorms in the afternoon. Some thunderstorms may produce gusty winds, and heavy rainfall in the afternoon. Highs in the upper 60s. Southwest winds 10 to 15 mph. Chance of rain 90 percent.
Mostly cloudy. Showers likely with a chance of thunderstorms in the evening. Lows in the lower 40s. West winds 10 to 15 mph with gusts up to 25 mph. Chance of rain 70 percent.
Sunny. Much cooler with highs in the mid 40s.
Mostly clear in the evening...then becoming mostly cloudy. Cooler with lows in the mid 20s.
Mostly cloudy with a 30 percent chance of light snow. Highs in the lower 30s.
Partly cloudy in the evening...then becoming mostly clear. Lows 15 to 20.
Partly sunny. Highs in the mid 30s.
Partly cloudy. Lows in the upper 20s.
Partly sunny. Not as cool with highs in the lower 50s.
Partly cloudy in the evening...then becoming mostly cloudy. Lows in the mid 30s.
Partly sunny. A chance of showers in the afternoon. Highs in the mid 50s. Chance of rain 40 percent.
Doppler Radar Map for New Jersey
This is the latest Doppler Radar Map for New
Jersey from the National Weather Service. This image is generated at
the National Weather Service's Mount Holly, New Jersey station by
NEXRAD (Next Generation Radar) obtains weather
information (precipitation and wind) based upon returned energy. The
radar emits a burst of energy (green). If the energy strikes an object
(rain drop, bug, bird, etc), the energy is scattered in all directions
(blue). A small fraction of that scattered energy is directed back
toward the radar. This reflected signal is then received by the radar
during its listening period. Computers analyze the strength of the
returned pulse, time it took to travel to the object and back, and
phase shift of the pulse. This process of emitting a signal, listening
for any returned signal, then emitting the next signal, takes place
very fast, up to around 1300 times each second.
NEXRAD spends the vast amount of time "listening"
for returning signals it sent. When the time of all the pulses each
hour are totaled (the time the radar is actually transmitting), the
radar is "on" for about 7 seconds each hour. The remaining 59 minutes
and 53 seconds are spent listening for any returned signals. The
ability to detect the "shift in the phase" of the pulse of energy makes
NEXRAD a Doppler radar. The phase of the returning signal typically
changes based upon the motion of the raindrops (or bugs, dust, etc.).
This Doppler effect was named after the Austrian
physicist, Christian Doppler, who discovered it. You have most likely
experienced the "Doppler effect" around trains. As a train passes your
location, you may have noticed the pitch in the train's whistle
changing from high to low. As the train approaches, the sound waves
that make up the whistle are compressed making the pitch higher than if
the train was stationary. Likewise, as the train moves away from you,
the sound waves are stretched, lowering the pitch of the whistle. The
faster the train moves, the greater the change in the whistle's pitch
as it passes your location. The same effect takes place in the
atmosphere as a pulse of energy from NEXRAD strikes an object and is
reflected back toward the radar. The radar's computers measure the
phase change of the reflected pulse of energy which then convert that
change to a velocity of the object, either toward or from the radar.
Information on the movement of objects either toward or away from the
radar can be used to estimate the speed of the wind. This ability to
"see" the wind is what enables the National Weather Service to detect
the formation of tornados which, in turn, allows them to issue tornado
warnings with more advanced notice.