Sentence examples for mean annual stream from inspiring English sources

From 2004 to 2010 mean annual stream temperature (Ts) was elevated 0.8 2.1 °C in the burned and post-fire salvage logged streams compared to the unburned streams.

The results indicate that there were two primary spatial driving forces of wetland change in Peru's Cordillera Blanca from 1987 to 1995: 1) loss in glacier area was associated with increased wetland area, controlling for other factors; while 2) an increase in mean annual stream discharge in the previous 12 months increased wetland area.

Our preferred model combines the weight of 6 factors (i.e. slope gradient, land cover, mean annual precipitation, stream density, proximity to roads and slope orientation).

The mean annual in-stream chloride concentration equation uses readily available spatial data – with province-wide coverage – that can be easily used in any urban watershed.

The mean stream length is directly related to mean annual runoff; therefore, the highest mean stream length has relatively high mean annual rainfall runoff and relatively low mean annual rainfall runoff in less mean stream length.

Conservative tracer tests conducted in the Truckee River, a stream with mean annual discharge >0.5 m3 s−1, were simulated with both one (1-SZ) and two-storage zone (2-SZ) transport models to quantify the relative role of surface transient storage (STS) and hyporheic transient storage (HTS) on the physical transport of solutes in a large stream.

These attributes included mean stream elevation, mean January minimum air temperature, and mean July maximum air temperature, mean stream gradient and mean annual precipitation.

Factors considered to be potential controls of slope failure within this area include slope gradient, rock type, distance from roads, slope orientation, mean annual precipitation, soil type, land cover type, stream density and distance from stream.

For streams, the five best single predictors of water chemistry were the amount of arable land in the catchment (68%), followed by the amount of alpine treeless areas in the catchment, altitude (2.7%), stream width (2.7%), and mean annual discharge Q (1.3%).

In the present study, mean stream length is indicating the high mean annual rainfall runoff.

Regression tree analysis determined that the highest percentages of stream burial occurred in catchments characterized by higher mean annual precipitation (>990 mm), coarser soil types and extensive agricultural land use (>79.7%).