Fire Weather Watch
2025-12-20T00:00:00-07:00

...CRITICAL FIRE WEATHER CONDITIONS THURSDAY AND FRIDAY... Strong northwest winds will spread across the northeast plains after sunrise today, with gusts 45 to 65 mph creating critical fire weather conditions despite somewhat marginal humidity values near 20%. Early Friday, westerly downslope winds will bring strong gusts to the Front Range mountains and foothills, with potential for these to spread into wind-favored portions of the adjacent lower elevations. Peak gusts of 70-90 mph are increasing in likelihood for the windiest locations (considerably lower for areas along and east of I-25). With a warmer and drier air mass in place, humidity values in the teens look to extend into much of the foothills, and certainly across the lower elevations. Such conditions may be a longer duration than usual, with potential for low humidity to extend into the evening hours prior to the arrival of a front. The National Weather Service in Denver has issued a Fire Weather Watch for wind and low relative humidity, which is in effect from Friday morning through Friday evening. * AFFECTED AREA...Fire Weather Zones 215, 216, 241, 243, 245, 246 and 247. * TIMING...From Friday morning through late Friday evening. * WINDS...West 25 to 35 mph with gusts up to 80 mph in and near the foothills. West 15 to 25 mph with gusts up to 45 mph for areas roughly along and east of I-25. * RELATIVE HUMIDITY...As low as 10 to 15%. * IMPACTS...Conditions will be favorable for rapid fire spread. Avoid outdoor burning and any activity that may produce a spark and start a wildfire.


Blackwater River River Levels

Last Updated: December 18, 2025

The Blackwater River is a 65-mile-long river located in West Virginia.


Summary

Total streamflow across the Blackwater River was last observed at 499 cfs, and is expected to yield approximately 990 acre-ft of water today; about 22% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 2,222 cfs, with recent peaks last observed on 2013-06-04 when daily discharge volume was observed at 22,386 cfs.

Maximum discharge along the river is currently at the Blackwater River Near Franklin reporting a streamflow rate of 253 cfs. However, the streamgauge with the highest stage along the river is the Blackwater River Near Dendron with a gauge stage of 32.56 ft. This river is monitored from 9 different streamgauging stations along the Blackwater River, the highest being situated at an altitude of 3,138 ft, the Blackwater R Nr Davis.

River Details

Last Updated 2025-12-18
Discharge Volume 990 ACRE-FT
Streamflow 499.0 cfs
-97.8 cfs (-16.39%)
Percent of Normal 22.46%
Maximum 22,386.0 cfs
2013-06-04
Seasonal Avg 2,222 cfs
       
River Streamflow Levels
Streamgauge Streamflow Gauge Stage 24hr Change (%) % Normal Minimum (cfs) Maximum (cfs) Air Temp Elevation
Blackwater R Nr Davis
USGS 03065400
132 cfs 1.81 ft
Blackwater R At Davis
USGS 03066000
109 cfs 2.13 ft 101.85
Blackwater River Near Rocky Mount
USGS 02056900
56 cfs 1.93 ft -17.9
Blackwater River At Blue Lick
USGS 06908000
27 cfs 6.83 ft 2.69
Blackwater River Near Webster
USGS 01087000
19 cfs 1.91 ft
Blackwater River Near Bradley Al
USGS 02369800
36 cfs 0.67 ft -2.7
Blackwater River Nr Baker
USGS 02370000
68 cfs 1.1 ft -1.59
Blackwater River Near Dendron
USGS 02047500
137 cfs 32.56 ft 0
Blackwater River Near Franklin
USGS 02049500
253 cfs 4.09 ft -5.6
Seasonal Discharge Comparison
Maximum Streamflow Discharge
Streamflow Elevation Profile

A blackwater river is a type of river with a slow-moving channel flowing through forested swamps or wetlands. As vegetation decays, tannins leach into the water, making a transparent, acidic water that is darkly stained, resembling tea. Most major blackwater rivers are in the Amazon Basin and the Southern United States. The term is used in fluvial studies, geology, geography, ecology, and biology. Not all dark rivers are blackwater in that technical sense. Some rivers in temperate regions, which drain or flow through areas of dark black loam, are simply black due to the color of the soil; these rivers are black mud rivers. There are also black mud estuaries.
Blackwater rivers are lower in nutrients than whitewater rivers and have ionic concentrations higher than rainwater. The unique conditions lead to flora and fauna that differ from both whitewater and clearwater rivers. The classification of Amazonian rivers into black, clear, and whitewater was first proposed by Alfred Russel Wallace in 1853 based on water colour, but the types were more clearly defined by chemistry and physics by Harald Sioli (de) from the 1950s to the 1980s. Although many Amazonian rivers fall clearly into one of these categories, others show a mix of characteristics and may vary depending on season and flood levels.