The hydrology of the watersheds is regulated by the seasonal influences of a temperate climate, with its maximum flows occurring during snowmelt and its’ minimum flows occurring during base flow in late summer.
The Wild River is the only tributary to have its highest discharge for the period of record to take place in the 2010 water year; the remaining tributaries had their highest discharge for the period of record take place in other water years: 2004 water year for the Nezinscot River and 2011 water year for the Little Androscoggin River and Ellis River. All four tributaries had their lowest discharge for the period of record to take place in the 2002 water year.
The Wild River had an average discharge of 246 ft3/s; a minimum discharge of 6 ft3/s; a maximum discharge of 8181 ft3/s; a
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For the 2010 water year, more than a dozen precipitation events can be observed; the three most distinctive were: (1) the normal snowmelt (2) early December 2010, heavy precipitation and combine with warm temperatures resulting in minor flood for the area and (3) Tropical Storm Irene in late August 2011. The watershed hydrology behavior normal, with its highest flows during snowmelt and its lowest flow occurring during baseflow (see Graph 10).
All four tributaries had their highest discharge values during a January storm combine with warming temperatures resulting in snowmelt and their lowest discharge values during base flow in the summer months.
The Wild River had an average discharge of 154 ft3/s; a minimum discharge of 9 ft3/s; a maximum discharge of 5463 ft3/s; a range of 5453 ft3/s; a maximum/minimum ratio of 589 ft3/s and a standard deviation of 394 with a coefficient variation 2.56 (see Table
On May 19 and 20, 1990, terribly significant rains fell within the river Basin, particularly over the lower finish of Lake Hamilton and far of Lake Catherine. within the twelve-hour amount from 6:00 p.m. May 19, 1990 to 6:00 a.m. May 20, 1990, there was downfall of 10 inches at Carpenter Dam, seven inches at Remmel Dam, and twelve inches in near Hot Springs, with most of the rain falling between 8:00 p.m. and 3:00 a.m. The pool elevation on Lake Hamilton was 399.16 feet higher than water level at 8:00 p.m. on May 19, however when four hours, had up to 402.12 feet, and was still rising. Throughout this point the gates on Carpenter Dam were opened so as to avoid flooding on Lake Hamilton. The mixture of the discharge from Lake Hamilton and therefore the influx of rain from Lake Catherine's catchment area flooded the shores of Lake Catherine. The tail water from Carpenter Dam rose from a traditional elevation of 305 feet, to an elevation of 331 feet by 4:00 a.m. on May 20. Before the flooding, the pool elevation at Remmel Dam was close to traditional at 304.33 feet, however the pool at Remmel Dam crested at 7:00 a.m. on May 20th at 4:00am at an elevation of 317.50
A mass curve and double mass curve were created for the Red Deer basin at Drumheller in 1964. Precipitation data was collected from the city of Drumheller, which is approximately 0.6 km from the river measurement. On average the greatest amount of precipitation occurred in May, June, and July, but there was a large spike in precipitation in the month of September. The lowest amount of precipitation occurred in January, February and October. The double mass curve for this basin has a large gradual increase. Runoff for this basin is always greater than precipitation, but there is an area of large run off and storage during the end of the curve. This could be due to the large amount of precipitation that occurred in September, and storage
The Watershed Management Program relies upon the Four Mile Run Computer Model to simulate the watershed 's complex hydrology and the impacts of stormwater runoff from local land use changes and drainage modifications. The impacts of a proposed project are reviewed and corrective measures are recommended if the model predicts flooding problems in the lower Four Mile Run.
4. Compare snowpack in a watershed to a dam on a river. How are they alike? How are they different?
Lenz, ( 2003 ) studied the Ground-Water Flow and Rainfall Runoff with Emphasis on the Effects of Land Cover, Whittlesey Creek, Bayfield County, Wisconsin, 1999-2001 using SWAT model. The effects of land cover on flooding and base-flow characteristics of Whittlesey Creek, Bayfield County, Wis were examined in a study that involved ground-water-flow and rainfall-runoff modeling. Field data were collected during 1999-2001. Potentiometric-surface altitudes and stratigraphic descriptions were provided by well logs. Geological data, soil parameters, hydrography, altitude, and land-cover data were compiled into a geographic information system (GIS) and used in two ground-water-flow models (GFLOW and MODFLOW) and a rainfall-runoff model (SWAT). A base flow of 17-18 cubic feet per second is produced in a deep ground-water system which intersects Whittlesey Creek near the confluence with the North Fork.
Fortunately, that same weekend a series of powerful thunderstorms swept over the northern Sierra flows ever so slightly elevated in the Yuba and Feather Rivers. This fortuitous event could not have come any sooner because coincidently, that week in August was just after the downstream demand curve had peaked and the ever so slight bump in flows had knocked the final round of curtailments
This segment of White Creek is located the farthest away from major urban development, and, thus, might be an overall healthier system as a result. There is an overall proliferation of many different of species (colonizers, stabilizers, and riparian woody) that occur and thrive in various spatial configurations (partially determined by proximity to stream, elevation, and characteristics of the underlying substrate). There appears to be a substantial (s worthy of note that a large, above-ground sewage line ran perpendicularly over the river towards a sewage treatment plant some distance away. There were no signs of leakage or other issues that might compromise or affect the surrounding hydrology of the site.
The overall goal of my research is to better understand the roles that fatty acid binding proteins (FABPs), specifically epidermal-FABP (FAPB5) and brain-FABP (FABP7), play within regulating the endocannabinoid system and to understand the role of FABP in addiction. The endocannabinoid system is linked with the rewarding effects of abused drugs. Central to the endocannabinoid system is the cannabinoid type 1 receptor (CB1R), which is expressed ubiquitously throughout the brain. Within the brain reward circuit, activation of CB1Rs regulates the strength and plasticity of glutamate and GABA synapses. Specifically, dopaminergic projections from the ventral tegmental area (VTA) to the nucleus accumbens (NAc) plays a critical role in reward
The average yield of total nitrogen between the two rivers differ. The Red River has a slightly higher nitrogen yield in the early data set (1992-1994) than the Sweetwater River (Figure 2A). Whereas, nitrogen yield in the Red River is significantly lower than the Sweetwater in 2005-2007 (Figure 2A). Comparing the two datasets corresponding to years, the Red River showed significant decrease in the average yield of nitrogen (Figure 2A). However, the Sweetwater nitrogen yield has dramatically increased since the earlier data collection (Figure 2A).
Two charts were used, one from 2006 and the other from 2007. In 2006 it was considered a wet year meaning a greater percentage of 41% of the water went to wild and scenic rivers. In 2007 it was a dry year which greatly reduced the percentage to only 23% going to wild and scenic
There were a total of 111 days of rainfall within the year preceding the dam’s failure. This level of rainfall was very unusual for the community of Johnstown, let alone the entire state of Pennsylvania. Just before the dam broke, 6-8 inches of rain had fallen throughout the region, turning
The Department of Water Resources every year collects snowfall and rainfall data . On April 1st California’s snowpacks are usually the highest , but “ the water content measurements of this year's snow were only about 5 percent of the usual rainfall “ ( la times ) . Which estimated that the year this data was taken would be the lowest on record .
The maximum snow depth reaches up to 1500mm (Matsumura, 2014). The maximum hourly rainfall occurred is 32mm on 04-09-2013. The slope failure has happened on 17-10-2013. 47mm of daily cumulative rainfall has been observed during 16-10-2013. In this case, the slope failure has also been influenced by the excess amount of water supply (approximately 1m3/day). The monitored data i.e. rainfall, snow depth, soil water content and pore water pressure are given in Fig.3(a).
Most of us may ask our self, what ages does schizophrenia start to develop and who get this disorder? Well most of who get them are the man than women’s. Faustman suggests, “that even that may represent the risk factor for schizophrenia occurs in life or even before birth”. The essence of faustman’s argument is that some children may have already developed schizophrenia before he/she was born. Schizophrenia occurs in all national groups around the world. According to the national institute of mental health, “Symptoms such as hallucinations and delusions usually start between 16 and 30. Males tend to experience symptoms a little earlier than females”. In other words, most suffer from schizophrenia occurs in late adolescence and early adulthood.
1. Women in Ancient Greece Mention ancient Greece to a friend and they may think of democracy, the Olympic games or the Spartan army. However, men created many of the sources that tell us about these institutions and developments; men were also the intended audience (Scott, 2009). But the ancient Greeks still felt a female presence in many aspects of their culture, including female gods, characters in poetry and folklore, and of course in everyday life. Women in the city of Sparta were allowed to own land, and one of the Spartan kings’ sisters even entered a chariot team in the Olympic games of 396 and 392 BCE (Scott 38).