![]() |
||
| Selected %: | 2% | 5% | 10% | 20% | 50% | 80% | 90% | 95% | 98% |
| 0.339 | 0.419 | 0.526 | 0.674 | 0.941 | 1.304 | 1.545 | 1.76 | 2.01 |
The top row is the "non-exceedance probability" and the second row is the ratio of the precipitation for the non-exceedance probability in that column to average precipitation. Remembering that you selected a 2 month duration starting in June on the "Interface" page, this table tells you that there is a 5% chance that June-July precipitation will not exceed 0.419 of average precipitation for June-July. Some people would invert the 5% and say that the region was experiencing a 20 year drought if it were to receive 0.419 of average precipitation in the June-July period. You can see there is a 10% chance of getting at least 0.526 of average precipitation for the period. Since the region received 45% in this example, you can answer the question "How rate is the current drought" by saying: the odds of having a June and July this dry in central Alabama are a little more than 5% (or) we can expect a drought like this at least every 10 years on average (or) (interpolating graphically) we can expect a drought like this about every 15 years on average If you find the "once every 10 years" expression makes more sense to people, remind them that this does not mean that the drought occurs on a 10 year cycle, just that if you examined precipitation records for a very long period of time, about one in 10 of those years would have less June-July precipitation. Another dimension of drought is streamflow, which is of special importance from the standpoint of reservoir inflow, wastewater effluent dilution, and fish survival. It is usually the case that the frequency of occurrence of streamflow is not the same as the frequency of occurrence of the precipitation that generated the streamflow. It could be more or less frequent. Streamflow frequency is approached in essentially the same manner as precipitation. Use the streamflow regions selection map, and download the appropriate regional spreadsheet. But note that there is no regional analysis of streamflow stations, and you must compare current data for a station listed in the Atlas spreadsheet to the statistics for that station. Considering that watersheds above gauging stations have different drainage areas and land use, the frequency of occurrence of flows at nearby stations might be quite different. Return to Main Page, National Drought Atlas Precipitation Streamflow.
revised 1 Aug 2006