Sentence examples for excess precipitation from inspiring English sources

We observe that ERA-Interim excess precipitation induces a fresh bias in the surface salinity response.

In comparison, excess precipitation regions show strong negative correlations with drought indicators in most growth stages.

Unlike surface reservoirs, aquifers are not subject to evaporative loss, but under natural conditions they are only recharged slowly as excess precipitation percolates into the aquifer.

Excess precipitation of MX type particles relatively weakens the grain boundaries as compared with the matrix and, as a consequence, lowers the rupture strength.

In the mid-1990s' mid-1990s'orial intheannual variability is dominatequatorialonth perinterannualwhich exhibit the structure observariabilityl coupled ocean–atmosphere warm events (zonal wisdominatedweakening and zonal surface slope relaxation, warm SST, excess precipitation).

The CO2 flux from the water surface to the atmosphere during a flood event is three times greater than during base flow, suggesting that excess precipitation flushes soil organic carbon to the river through interflow and enhances the loss of terrestrial carbon via river water to the atmosphere.

Groundwater flow and discharge from springs may provide additional water input, but evaporation rates are always in excess of precipitation and surface runoff.

An excess of precipitation over evapotranspiration (ET) plus runoff contributes to an increase of TWS.

The predominance of overland flow-related sedimentary deposits suggests an excess of precipitation over evaporation that influenced local palaeohydrology.

The deuterium excess in precipitation (d = δ2H – 8 × δ18O) is usually construed as an isotope signal dependent on climate conditions during evaporation.

The isotopic composition and deuterium excess of precipitation samples are directly and inversely proportional to temperature, respectively.