Tag Archives: river levels

“Flood Information” page now available

According to our access logs, we are getting (ahem) inundated by searches for flood-related information. We can take a hint. Check out the navigation bar up there at the top of this page. The NFPA web site now has a dedicated Flood Information page containing links to such things as river levels, snowpack data and forecasts.

Truth be told, putting this together was a bit of a nuisance. At least three different federal agencies maintain relevant and sometimes overlapping information. The Flood Information page has a good set of starter links. We’ll add more as we find them.

Current and forecast river levels available online

For those of you who wish to keep an eye on things, the National Weather Service has graphics displaying current and forecast river levels available online.

If necessary, scroll down the page a little ways to see the North Fork data. There are three automated gauges on the North Fork Flathead: at the Canadian border, at Polebridge and at Columbia Falls. With exceptionally bad timing, the gauge at Polebridge is down right now, but presumably will be fixed fairly soon.

Link: WFO Missoula Composite Hydrograph Page

Flooding in Northern Rockies expected to start this week

A warming trend later this week is expected to increase snowpack runoff and likely cause small stream flooding by Friday.

The Daily Inter Lake has the story . . .

The National Weather Service expects mountain snowpack to begin melting at a more rapid rate beginning Wednesday and extending through Friday, according to a weather outlook released Saturday afternoon.

A ridge of high pressure is forecast to bring warmer air to the Northern Rockies, increasing the likelihood that small streams and creeks will spill out of their banks by Friday.

The warmer weather system is expected to come on the heels of persistent rain and snowfall today and Monday at elevations above 6,000 feet, where snow levels are already well above historic averages.

Continue reading . . .