This river stands between latitude and longitude 32°22′ to 33°52′N and 48°15′ to 49°E, respectively.
The majority of c-q studies involve non-urban areas in environmental settings such as the subtropics, mountains, and high latitude rivers.
Field measurements were carried out in forests of various states of disturbance from 2015 wildfires surrounding the confluence of the Yukon and Tanana Rivers (near 65°8′N latitude, 152°27′W longitude), about 200 km west of Fairbanks, Alaska.
We conducted an AMOVA considering only coastal and Andean river basins within latitudes 34°S and 40°S in Chile.
We quantified the composition and spatial configuration of seascapes and calculated coastline length, number of estuaries, river length and geographical latitude using 12 metrics within ninety 30-nautical-mile grid cells, which supported inshore fish catch data from 21 species groups.
To examine the effects of latitude, wind and river discharge on the river plume, we designed several numerical experiments.
Here, we apply a numerical model to the Upper Gulf of Thailand (UGoT) to examine a river plume in low latitudes.
Martian waters slowly dissipated to space, and the disfiguring Tharsis lump pulled the dying planet over, carrying the abandoned river valleys to foreign latitudes.
This chapter discusses the hydrology of rivers at high latitudes, which includes all freshwater flows to the Arctic Ocean and northern seas.
Two major controlling factors are suggested: low differential of energy between small and large floods, peculiar to low energy rivers of mid-latitude, and low critical discharges for lateral erosion and bedload mobilization.
