Sample Resume : Underground Hydrological Cycle Essay

Surface water commonly is hydraulically connected to ground water, but the interactions are difficult to observe and measure (Winter, 1998). Interaction depends upon understanding the effect of topography, geology and climate of the groundwater

The state of Michigan is a fascinating area. From its mitten-like shape, to its historical background, to the presence of the Great Lakes, Michigan has a story unlike any others. One very important part of Michigan’s story is how water has shaped the land making up the state. Seeing as the Great Lakes surround Michigan, it is obvious that the hydrologic system plays a great role in the water supply and the ecosystem of the Great Lakes. The hydrologic cycle includes evaporation, condensation, precipitation, groundwater, transpiration and runoff, all of which keep the Great Lakes functioning year after year. The University Corporation of Atmospheric Research developed an image to simply explain the hydrologic cycle as well as graphs explaining how each of the elements of the hydrologic cycle affects The Great Lakes on a monthly basis (located below).

This photo journal assignment was very interesting and educational. It helped me look outside the box and to really relate geography to my everyday life. My first relatable topic that I came in contact with during this assignment was the process of evaporation. At Dry Creek park in Modesto, CA, I witnessed evaporation taking place in the creek. I have been going to this park for quite some time and in the summer, water levels decrease drastically. Evaporation is one of the four phases in the hydrologic cycle (water cycle). According to our Geosystems Eighth Edition book, Christopherson say, “Water travels endlessly through the hydrosphere, atmosphere, lithosphere and biosphere. [...] Currents of water, vapor, ice and energy are flowing

The Denver Basin aquifer framework is a noteworthy wellspring of water for South Metro Denver. The system extends from Colorado Springs in the south to Greeley in the north, from the foothills close to Golden in the west, toward the eastern fields close to Limon, is a surface locale of around 6,700 square miles. It joins four aquifers: the Dawson, Denver, Arapahoe, and Laramie-Fox Hills. Each aquifer has different water quality, profundities, and water availability (CFWE, 2002).

The Denver Basin aquifer framework is a noteworthy wellspring of water for South Metro Denver. The system extends from Colorado Springs in the south to Greeley in the north, from the foothills close to Golden in the west, toward the eastern fields close to Limon, is a surface locale of around 6,700 square miles. It joins four aquifers: the Dawson, Denver, Arapahoe, and Laramie-Fox Hills. Each aquifer has different water quality, profundities, and water availability (CFWE, 2002).

The Denver Basin aquifer framework is a noteworthy wellspring of water for South Metro Denver. The system extends from Colorado Springs in the south to Greeley in the north, from the foothills close Golden in the west toward the eastern fields close Limon, a surface locale of around 6,700 square miles. It joins four aquifers: the Dawson, Denver, Arapahoe, and Laramie-Fox Hills. Each aquifer has different water quality, profundities, and water availability (CFWE, 2002).

Problems encountered throughout the water cycle is from the excess water flowing into drainage systems thus causing -

It is considered by scientist, that all ground and surface waters are deemed to have hydrological connection, and characterized as: (a) surface water; (b) diffused surface water; (c) groundwater; (d) percolating groundwater. In governing the use of water, various rules and regulations have been developed for each classification.

Water storage can be either fresh water or salt water. Ground water is where there is just a body of water, or water that is on the ground. Also water storage does not have to be in liquid form. It can be found in snow, ice, or glaciers. When one of the solid forms of water melts it is called run off water. When run off water runs into a water storage it will evaporate at some point in the future.

Beautification is not the only challenge we faced, as another major problem of the backlot is stormwater. This is the water created by storms. When solving this problem, we first learned about the water cycle, and how water interacts with the earth. We saw that water gathers in certain

The transient simulation was carried out to simulate the behavior of the aquifer in response to climatic change in the dry period after decreasing the infiltration rate with the end of the last wet period (~10,000 yr BP). The calibration in this stage was used the groundwater contour lines measured by Ball (1927) and Sandford (1935) which represents the groundwater level in the aquifer before beginning of the heavy exploitation in 1960 neglecting the very low decline in the water level between 1935 and 1960 in comparison to the long period between 10,000 BP and 1927 or 1935

Drylands in the western United States are subject to generally low soil moisture content. Understanding the hydrology and moisture levels of these soils is crucial to understanding dryland ecosystems (Newman et al. 1997 Journal of Hydrology; Wythers et al. 1999 SSSAJ). Soil water is lost through bare-soil evaporation and transpiration (Wythers et al. 1999 SSSAJ). Commonly, these processes have been linked together as evapotranspiration; distinguishing between the two is a difficult yet important task (Villegas et al. 2010 Journal of Arid Environments; Wythers et al. 1999 SSSAJ). One way to better estimate evapotranspiration and understand the water budget in drylands is to determine the processes driving soil evaporation. It

Precipitation is the third step in the water cycle. The water cycle is a process in which water circulates between the Earth’s oceans, atmosphere, and land. The water cycle involves precipitation such as rain, snow, drainage in streams and rivers, and then returns to the atmosphere by evaporation and transpiration. Evaporation is when the sun heats up the water in rivers, lakes, or oceans and turns it into vapor or steam (Guenther, 1998-2015). The water vapor or steam will leave the river, lake, or ocean and will go into the air. Condensation occurs when water vapor in the air gets cold and changes back into

After traveling over 9000 miles, and accruing numerous scars and bruises, my image now reflects my passion. An insatiable hunger for knowledge and life-altering experiences take me across the world to environments which are worlds apart; the spectrum of ecosystems and complex webs of interaction that this exposes, only fuel my desire to continue exploring them. My research interests lie in Earth system relationships as well as human-environment interactions, and the cascading effects throughout nature and society alike. The principle which guides me through all of my experiences is the inter-connectivity of the natural world; working as an entomologist in the Swiss Alps, in

The Earth 's water is always in movement, and the water cycle, also known as the hydrologic cycle, describes the continuous movement of water on, above, and below the surface of the Earth. Since the water cycle is truly a "cycle," there is no beginning or end. Water can change states among liquid, vapor, and ice at various places in the water cycle, with these processes happening in the blink of an eye and over millions of years. Although the balance of water on Earth remains fairly constant over time, individual water molecules can come and go in a hurry, but there is always the same amount of water on the surface of the earth