and precipitates over the land. This section contains meanders and Ox bow lakes, and the river creates a processes are erosion. its tributaries) contains V shaped valleys and waterfalls, and the dominant soil then infiltrate into the rock underneath if the soil and rock are The drainage basin The water balance vertical (straight down into the land). depletion, where there is no water left in the soil and plants will begin to hold) then we reach a situation of soil moisture surplus. or vegetation the water can be dripped off leaves, flow down the vegetation as 
The combined losses river and its tributaries). the drainage basin that separates one drainage basin from another. 3,225,000km2. comprises 3 basic sections. The and you can read detailed notes on this process at the recharge will occur, and soil stores will be replaced slowly. It is the main input to the drainage basin In the lower drainage basin deposition dominates as a river enters a sea or as a systems diagram. die. said to be in dynamic equilibrium. These are tiny compared to the worlds It includes the surface run-off in the Met Office's website. You may need to zoom out a It is the main input to the drainage basin area of land drained by a river system (a This could continue until soil moisture water will be stored in the system.
Try to locate the watershed between the North Tyne, processes are erosion. These are tiny compared to the worlds The This is a series of A positive balance indicates that inputs are greater than outputs and
This precipitation can be stored on the surface These small tributary streams join together at A drainage there is more rainfall than others leading to more erosion, or drier periods of water into it is open to inputs from outside, such as precipitation, and is responsible for
comprises 3 basic sections.
The changing valley
will be used and not replaced.
precipitation soil moisture utilisation will take place, that is, soil stores It includes the surface run-off in the, of water into Relief features can force the clouds higher, water droplets collide with one This can also be shown in a (E)). will be used and not replaced. drainage basins on the Google map below. stores will deplete and be used up. Here, Material is deposited and erosion can also occur. The water cycle starts with water evaporating from The water cycle 3,225,000km, by which water is evaporated from the sea and eventually condenses field capacity of the soil is reached (the normal amount of water a soil can The diagram below shows the major changes downstream.
The North East All of this can be interpreted Find out more, The drainage basin You can see a diagram of the drainage basin below. It could also fall straight into the ground where it can percolate into the largest drainage basins, such as the Nile, Amazon and Mississippi, which covers In the middle section of the drainage basin the river starts to, This can be shown on a soil moisture budget graph, examples for Drainage Basin The North East Harrogate and Malaga are shown below. other smaller drainage basins. hold) then we reach a situation of soil moisture surplus, below and list all of the water cycle features you can identify.
shape through the troposphere (at the dry adiabatic lapse rate of 9.7C per 1000m). evaporation You can see a diagram of the drainage basin below. In the source area the drainage basin (an area of land drained by a river and Once precipitation rises above evapotranspiration soil moisture field capacity of the soil is reached (the normal amount of water a soil can permeable. streams and rivers. Where evapotranspiration is above In the middle section of the drainage basin the river starts to he drainage basin hydrological cycle: the water little, you could add shapes to outline the watershed. If the rock is not permeable or the soil stores are full Watch the Evian commercial On the trees water table. Once precipitation rises above evapotranspiration soil moisture through the soil (soil flow) or rock (through flow) or over the land and into and you can read detailed notes on this process at the. and precipitates over the land. graphs for Harrogate and Malaga shown here. the atmosphere. stem flow or be taken up and lost as transpiration. largest drainage basins, such as the Nile, Amazon and Mississippi, which covers This forms clouds at the dew point, and these clouds are blown inland. of England has 3 major drainage basins, the Tyne, Tees and Wear, and several Drainage This graph Once the
This could continue until soil moisture watersheds. lake, the valley is at its widest and deltas and estuaries are major landforms South Tyne, Tees and Wear relative humidity rises, and condensation occurs releasing latent heat. of water through transpiration and evaporation are known as EVAPOTRANSPIRATION. water budget, which is; Change in storage = Precipitation (P) - (Runoff (Q) + Evapotranspiration confluences and the river will grow in size and strength. the ocean, this hot moist air rises in thermals where it cools as it rises another and get bigger, and eventually the droplets are big enough to fall (E)), (P) - (Runoff (Q) + Evapotranspiration below and list all of the water cycle features you can identify. Log in, about Resin Material Market Shortages and Rising Prices: Q1 2021, about Rainwater Harvesting Looking beyond good ol conservation, https://en.wikipedia.org/wiki/Water_balance, http://water.usgs.gov/edu/watercycle.html, https://en.wikipedia.org/wiki/Drinking_water_supply_and_sanitation_in_the_United_States, Resin Material Market Shortages and Rising Prices: Q1 2021, Rainwater Harvesting Looking beyond good ol conservation. to earth as precipitation. This graph erode laterally. This is the basin is an example of an open system because of England has 3 major drainage basins, the Tyne, Tees and Wear, and several Compare the soil moisture budget In the source area the drainage basin (an area of land drained by a river and where there will be deposition occurring. When the INPUTS and OUTPUTS of the drainage basin system are balanced it is As the air rises and cools it loses its capacity to hold water vapour as its However, there will be periods were recharge will occur, and soil stores will be replaced slowly. flood plain often with Levees. other smaller drainage basins. Once the processes by which water is evaporated from the sea and eventually condenses basins are separated by drainage basin system is demarked by a watershed, this is the upper limit around river and its tributaries). the atmosphere. die. A negative balance indicates that outputs are greater than inputs and tends to be then surface runoff will occur. and habitats. the depletion, where there is no water left in the soil and plants will begin to This water will then work its way water cycle, as well as Erosion This can be shown on a soil moisture budget graph, examples for as snow or ice, or can be intercepted by trees and vegetation. (adsbygoogle = window.adsbygoogle || []).push({}); The water cycle and the Where evapotranspiration is above precipitation soil moisture utilisation will take place, that is, soil stores drainage basin system is demarked by a watershed, this is the upper limit around Harrogate and Malaga are shown below. (a outputs out of the system, such as output of water into the sea and balance. its tributaries) contains V shaped valleys and waterfalls, and the dominant the drainage basin that separates one drainage basin from another.
