While attention has rightly been focused on the massive rainfalls and flooding in Iowa and along the Mississippi river, conditions are quietly getting soggier in central and northern Missouri. In Linn County, a bit north of us, over 7 inches of rain fell in 4 hours; Locust Creek went up 20 feet in a few hours. The Chariton River has gone up 18 feet at Prairie Hill, and the Grand has gone up 25 feet at Chillicothe. These are both significant tributaries to the Missouri River, which has been hovering around moderate flood stage for a while now. As I write this on Thursday morning, the upper Missouri basin in eastern NE and western IA is being pounded by severe storms, central/northern Missouri has had wave after wave of heavy rainfall, and more is rotating into our area. We’ve had over 5″ in the last 24 hours, including 3″ in one hour, producing the highest streamflow we’ve seen on our property, and it continues to fall. We’re forecast for continued storms through the weekend, including severe storms and heavy rainfall Friday and Friday night.
At the moment, the Missouri is forecast to once again reach a stage height of 25′ at Jefferson City, well below the 1993 record of 38.3′ but enough to start flooding lower areas, and this forecast doesn’t include all the oncoming rain. It’s been cycling around that height for weeks now, so this is nothing new, but it’s a lot of water and continued heavy rains across the basin could keep the trend going. So far we’ve been fortunate that the rain pulses are just far enough apart to allow the Missouri to drop again before the next pulse arrives, but that may not last. Much of the region is saturated, and can’t hold much more. More and more folks are quietly saying that this reminds of them of ’93, when this just kept happening; the rain just kept coming and the rivers just kept rising. We’ll see. There’s a long way to go in the Missouri basin, but that’s what they thought in Iowa and along the Mississippi not that long ago.
As ex and current geologists with experience in rivers, we’re fascinated on a scientific level by these dynamics. There are many good websites to use when tracking these events, mostly those managed by the National Weather Service and the USGS. When using these, however, you’ll notice massive gaps in stream gage coverage; this is due to major budget cuts in river monitoring that have really hampered our ability to accurately study, track, and predict river behavior. Read coverage of the Iowa floods carefully, and you’ll find the experts bemoaning the cuts that have kept them from doing their job.
In any case, for an overall view of river conditions, visit http://water.usgs.gov/waterwatch/. This national map shows streamflow conditions for all gages monitored by the USGS, and you can click on a state to zoom in, then click on any gage to see recent conditions.
Another good site is the National Weather Service’s Advanced Hydrologic Prediction Center, which takes similar data to the USGS site and presents them in a slicker, more intuitive interface that really helps present conditions, as well as offering river stage forecasts. As above, click on individual gage sites to view graphs, data, and predictions. The link above is to the Kansas City forecast region that covers most of the central/northern Missouri area I wrote about above, but you can scroll in any direction through the country. Also, at any particular gage, scroll down to see a location map and table of how different gage heights affect the surrounding area. It’s a good way to get context for the river conditions.
Finally, as a way of documenting the wet conditions this spring and early summer, here’s a link to the National Weather Service’s 1-year rainfall data for St Louis. This is a live, daily-updated graph, so if you’re reading this months later in the archive it might not fit my description. But as of late June, you’ll clearly see that we spent most of the winter slightly dry, but around mid-March the rain just started falling and is now 12″ above average. The comparable temperature graph shows the cool side of this agriculturally terrible spring, which has hurt everyone from gardeners to grain spreads.
So for now we just wait, watch the streams rise, and pay attention. Our permanent raised beds are generally saving us from larger disaster, as they keep the roots of our plants above the accumulating water, but that only goes so far. When the soil stays constantly wet and never gets a chance to drain, it will start to stunt and hurt the plants, so we’re concerned. The biggest worry right now is our beautiful stand of 200+ heads of garlic, which is in the process of forming bulbs, only a few weeks from harvest. Garlic needs fairly dry conditions to do this properly, and can rot easily in overly wet conditions. A friend has already lost at least half her garlic to waterlogged fields, and we’re in danger. Losing this crop so close to harvest would really hurt. Overall, though, as I’ve written before, these conditions cement our commitment to developing an effective no-till, permanent raised bed farming method here, because in the long run it will insulate us as much as possible against these sorts of conditions that are causing even more trouble and damage for more equipment-dependent growers.