interception-is the store of water droplets by plant leaves as rainfall occurs; overland flow-describes water which runs downslope in unconcentrated form such as sheet floods,rills and rivulets._by Malcom kahonde
Surface flow and overland flow are related but not exactly the same. Surface flow generally refers to water that moves across the ground surface, including both overland flow and water from other sources like melting snow or rainfall that doesn't infiltrate the soil. Overland flow specifically describes the movement of water over the land surface when rainfall exceeds the infiltration capacity of the soil, leading to runoff. Thus, while all overland flow is surface flow, not all surface flow is classified as overland flow.
Interception in geography refers to the process by which precipitation is captured and stored by vegetation before reaching the ground. It plays a role in regulating the water cycle and affects how much water reaches the soil or runs off into rivers. Interception can vary depending on the type of vegetation, weather conditions, and land use.
To distinguish between two cell types, you can analyze their morphology under a microscope, noting size, shape, and arrangement. Additionally, specific staining techniques can highlight unique cellular structures or components, such as organelles or surface markers. Molecular techniques, like flow cytometry or immunohistochemistry, can also identify distinct proteins or genes characteristic of each cell type. Finally, functional assays can reveal differences in behavior or activity, further aiding in their classification.
The mouth is highly sensitive to viscosity because it helps with the detection of different food textures and consistency. Viscosity influences how foods flow and stick together in the mouth, affecting the overall mouthfeel and taste perception. This sensitivity is crucial for helping us distinguish between various food types and textures.
The border across which genes can flow between two populations is called a "gene flow barrier." This barrier can be physical, such as a mountain range or river, or it can be due to behavioral or ecological factors that limit gene exchange between populations.
Surface flow and overland flow are related but not exactly the same. Surface flow generally refers to water that moves across the ground surface, including both overland flow and water from other sources like melting snow or rainfall that doesn't infiltrate the soil. Overland flow specifically describes the movement of water over the land surface when rainfall exceeds the infiltration capacity of the soil, leading to runoff. Thus, while all overland flow is surface flow, not all surface flow is classified as overland flow.
Hortonian Overland Flow is characterized by pooling of water caused rainfall exceeding the rate at which water infiltrates the ground. It is most common in urban areas with paved surfaces.
Another name for surface runoff is overland flow.
Interception in geography refers to the process by which precipitation is captured and stored by vegetation before reaching the ground. It plays a role in regulating the water cycle and affects how much water reaches the soil or runs off into rivers. Interception can vary depending on the type of vegetation, weather conditions, and land use.
Human causes of overland flow include urbanization, which increases impervious surfaces like roads and buildings, preventing water from infiltrating into the ground; deforestation, which reduces vegetation that helps absorb and slow down water; and poor land management practices such as excessive tilling or removal of natural water-absorbing features like wetlands. These activities can exacerbate overland flow and lead to increased flooding and erosion.
Some famous hydrologists include Luna Leopold, whose research revolutionized the field of fluvial geomorphology, and Walter Langbein, who made significant contributions to the study of groundwater flow. John Wesley Powell is another notable hydrologist, known for his exploration of the Colorado River and his work on water resource management in the western United States.
The surface flow is of two types 1. saturated flow, which is caused due to saturation of soil and 2. Hortonian flow, which is caused due to excess rainfall intensity. When the rainfall intensity exceeds the infilatration capacity of the soil, Hortonian flow takes place.
A heat conductor allows heat to flow easily through it due to the movement of free electrons, such as metals. An insulator, on the other hand, inhibits the flow of heat due to the lack of free electrons or tight bonding between atoms, such as rubber or wood.
DSS is more focused on senior management/leadership influencing strong company direction, and decisions. MIS focuses on information flow relationships.
Arterioles are smaller vessels that carry blood away from the heart, while venules are smaller vessels that carry blood back to the heart. By observing the direction of blood flow and the presence of valves (which venules have), one can distinguish between arterioles and venules in the frog's foot vasculature.
businesses purchase what they use to produce goods and services. Resources are in the form of labor, natural resources, capital, and entrepreneurship, all of which are supplied by households.
difference between laminar air flow & reverse laminar air flow