The phrase "a specific hydrologic" is correct and usable in written English.
It can be used when referring to a particular aspect or characteristic related to hydrology, such as in scientific or technical discussions.
Example: "The study focuses on a specific hydrologic model to predict water flow in the region."
Alternatives: "a particular hydrologic" or "a distinct hydrologic".
This paper summarizes how by applying factor analysis techniques to complete a statewide regionalization for Minnesota, hydrologic regimes were identified, each with a specific hydrologic signature; varying between three and four runoff periods of different durations.
The traditional approach in the hydrologic sciences and engineering fields has been to either treat the atmosphere as a forcing condition on the hydrologic model, or to adopt a specific hydrologic model design in order to be interoperable with a climate model.
Vanacker et al. (2003) proposed a methodology to investigate the effect of land use/land-cover change on slope movement susceptibility by incorporating specific hydrologic parameter estimates, in a simple process-based slope stability model.
A review of the existing literature shows that it is rich with descriptions of how beaver activities influence specific hydrologic and geomorphic processes.
We conclude that spatial descriptions of ecological processes in the fluvial landscape, constrained by their specific hydrologic and ecological dynamics and by the ecosystem matrix for interactions, i.e. the directional dispersal embedded in fluvial and host/pathogen mobility networks, have already produced a remarkably broad range of significant results.
Measurements from continuously deployed specific conductance sensors were recorded at least every hour and as frequently as every 5 min depending on the individual site and specific hydrologic conditions.
The hydrologic model HEC-HMS (Hydrologic Engineering Center, Hydrologic Modeling System), used in combination with the Geospatial Hydrologic Modeling Extension, HEC-GeoHMS, is not a site-specific hydrologic model.
Floodplains are depositional features of a channel valley associated with a specific climatic and hydrologic regime of a drainage basin.
In previous work, we have demonstrated that a specific sequence of hydrologic conditions, spring drought followed by continued summer rainfall, is critical for the amplification and transmission of both SLEV and WNV in south Florida [32], [36] [39].
In a series of articles, we have demonstrated that a specific sequence of hydrologic conditions, spring drought followed by continued summer rainfall, is critical for the amplification and transmission of both SLEV and WNV in south Florida (31, 35 – 35 ).
Such basic information on the drainage structure of an area can be valuable for site-specific hydrologic assessments but also has significant implications for critical loads assessment, as low runoff systems tend to be less buffered and therefore are more sensitive to acidification.
