The drainage basin includes all the surface water from rain runoff, snowmelt, hail, sleet and nearby streams that run downslope towards the shared outlet, as well as the groundwater underneath the earth's surface.
The hydrological cycle in a small river basin refers to the continuous movement of water from the basin's surface water, groundwater, and atmosphere. It involves processes such as evaporation, condensation, precipitation, infiltration, and runoff, which work together to circulate and distribute water throughout the basin. This cycle plays a crucial role in maintaining the water balance and ecosystem health of the small river basin.
Some of the major river basins in Nigeria include the Niger Basin Authority (mandate: cooperation, sustainable management of water resources), the Benue Basin Development Authority (mandate: development of water resources for agriculture, fisheries, and urban water supply), and the Ogun-Oshun River Basin Development Authority (mandate: water resources development for agriculture, domestic, and industrial use).
The agriculture in the Ganga-Brahmaputra basin is varied, with a focus on rice, wheat, jute, sugarcane, and tea cultivation. The region also supports a thriving fishing industry due to its extensive network of rivers and water bodies. Additionally, the basin is known for its fertile soil and diverse crop production.
The Amazon River basin in South America is a prominent example of a basin landform. It is a large low-lying area surrounded by higher elevations where the river and its tributaries drain and collect water. The basin supports a diverse ecosystem with high biodiversity.
The Orinoco watershed - its basin, covers an area of about 990000 km2
K. S. Ramasastri has written: 'Hydrological year book, ghataprabha sub-basin, 1988-89' 'Hydrological network for Tawi-J&K'
Factors that influence the operation of the hydrological cycle in a drainage basin include climate patterns, land use changes, topography, vegetation cover, and human activities like urbanization and deforestation. These factors can affect the infiltration, runoff, evaporation, and storage of water in the drainage basin, leading to changes in water availability and quality.
The hydrological cycle in a small river basin refers to the continuous movement of water from the basin's surface water, groundwater, and atmosphere. It involves processes such as evaporation, condensation, precipitation, infiltration, and runoff, which work together to circulate and distribute water throughout the basin. This cycle plays a crucial role in maintaining the water balance and ecosystem health of the small river basin.
An ungauged catchment is a river basin or watershed where no direct measurements of streamflow or hydrological data are available. This lack of data can complicate water resource management, flood forecasting, and environmental assessments. Techniques such as hydrological modeling, remote sensing, and regionalization of data from gauged catchments are often employed to estimate hydrological characteristics in these areas. Understanding ungauged catchments is crucial for sustainable water management and ecosystem conservation.
A drainage basin is an area of land where all surface water converges to a single point, such as a river or lake. It is also known as a watershed or catchment area, and it plays a crucial role in the hydrological cycle by collecting and channeling water runoff. The boundaries of a drainage basin are typically defined by the topographic divide, where water flows in different directions.
North Carolina is home to four major river basins that are unique to the state: the Neuse River Basin, the Tar-Pamlico River Basin, the Cape Fear River Basin, and the Yadkin-Peedee River Basin. Each of these basins has distinct ecological and hydrological characteristics, contributing to the state's diverse landscape. The Neuse and Cape Fear rivers are particularly significant for their economic and recreational importance.
The Ganga-Brahmaputra basin has varied topography due to its geological history, which includes the collision of the Indian and Eurasian tectonic plates, leading to the uplift of the Himalayas. This collision creates diverse landforms such as mountains, hills, and plains within the basin. Additionally, the region is shaped by erosion and sediment deposition from the rivers, resulting in fertile alluvial plains and intricate river systems. The interplay of these geological and hydrological processes contributes to the basin's rich topographical diversity.
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In Nigeria, the addresses of basins are typically categorized into major river basins, such as the Niger Basin, Benue Basin, and Chad Basin, each associated with specific geographical coordinates and administrative regions. Detailed information regarding these basins can be found in government reports, environmental studies, and resources from organizations like the Nigerian Hydrological Services Agency. For precise locations, maps and geographic information systems (GIS) databases can be consulted.
The passage of water through a drainage basin is primarily influenced by topography and soil characteristics. Topography determines the slope and shape of the land, affecting how quickly water flows over surfaces and into streams. Soil characteristics, including permeability and moisture retention, influence how water infiltrates the ground and moves through the subsurface. Together, these factors shape the hydrological dynamics within the drainage basin.
The development of the Amazon basin has resulted in extensive deforestation, loss of biodiversity, displacement of indigenous communities, and increased greenhouse gas emissions due to the clearing of forests for agriculture, logging, and infrastructure development. This has significant environmental and social impacts on the region and the global climate.
Anjali Bhat has written: 'Institutional and policy analysis of river basin management' -- subject(s): Brantas River Basin Development Project (Indonesia)