The Pascagoula River is formed in northwestern George County, just north of the Merrill community, by the confluence of the Leaf and Chickasawhay Rivers and flows generally southward through swampy bottomlands in George and Jackson Counties. In its lower course the river forms several channels and bayous; its largest such distributary is the West Pascagoula River, which flows into the Mississippi Sound at Gautier. The main channel passes Escatawpa and Moss Point and flows into the sound at Pascagoula. At low water the tidal effects are felt more than forty miles upstream.According to local Euro-American legend, the peace-loving Pascagoula tribe walked single file into the Singing River because the local Biloxi tribe were planning to attack. Anola, a Biloxi “princess”, eloped with the Pascagoula chief Altama, although she was engaged to a Biloxi chieftain. Anola’s angry would-be husband led his soldiers into battle with the Pascagoula. Outnumbered and fearing enslavement by the Biloxi, the tribe joined hands and walked into the river singing a death song. This section of the Pascagoula River became known as the “Singing River” because of this death song, which reportedly can still be heard at night.The water district manager has proposed the construction of a couple of dams on tributaries called the Big and the Little Cedar creeks to manage the river’s flow during a drought crisis. Since 1999 the water level in the river has fallen as low as 1.15 ft (on September 6, 2015) and 0.2 ft (October 8, 2000), as measured at the Graham Ferry gauge.
The Pascagoula River is a river, about 80 miles (130 km) long, in southeastern Mississippi in the United States. The river drains an area of about 8,800 square miles (23,000 km²) and flows into Mississippi Sound of the Gulf of Mexico. The Pascagoula River Basin is managed by the Pat Harrison Waterway District.
It is significant as the only unaffected (or nearly so) river with a discharge of over 10 cubic kilometres (2.4 cu mi) per year flowing from the United States into the Gulf of Mexico, and indeed the only one in the Cfa Köppen climate classification zone anywhere in the world, with the nearest approaches being the Juquiá and Itajaí in southeastern Brazil (The Yuan Jiang and Shinano Gawa are comparable to those Brazilian rivers but are only marginally in the Cfa zone). As a result, the Pascagoula has, in modern times, been the focus of a great deal of effort regarding its conservation to prevent the construction of dams on it.
George and Jackson counties, the two counties closest to the Gulf, have two separate wildlife management areas called Water trails that provide controlled recreation such as camping, birding, or canoeing.The higher water levels are partially due to events that occurred upstream. In the Upper Midwest, a record year of snow is now melting and flooding into waterways, such as the Mississippi River.
“When you’re talking about 15 barges all latched together, and you’re pushing it from behind, that becomes a very tricky endeavor when you’ve got really high degrees of current,” Steenhoeck told FOX Weather correspondent Nicole Valdes. “That can be quite, quite dangerous.”
By sending fewer barges down the river at a time, the pace of their deliveries may be slowed down – and in an industry involving perishable items, timing is everything.After months of low water levels, the Mississippi River now has the potential of having too much water, complicating the transportation of grain, soybeans and other crops on the river. During this time of year, Steenhoeck said, the ground behaves more like a tabletop than a sponge. This causes the water levels to recharge very dramatically in a very short period of time. The Mississippi River is an important avenue for delivering agricultural products from farms in the central U.S. to ports around the country and world.
The Diamond Lady, a once majestic riverboat, rests with smaller boats in mud at Riverside Park Marina in Martin Luther King Jr. Riverside Park along the Mississippi River on October 19, 2022 in Memphis, Tennessee.
Water levels along the Mississippi River near Memphis are more than 21 feet, which is nearly a foot higher than where they were in April 2023, according to the U.S. Geological Survey.For example, the river carried 93% of the cereal grain between Illinois and Louisiana, compared to 6% by rail, according to the Bureau of Transportation Statistics.
Why is the Pascagoula River called the Singing River?
The Singing River The Pascagoula is often called the “Singing River.” According to legend, the peace-loving Pascagoula Indian tribe sang as they walked hand-in-hand into the river to avoid fighting with the invading Biloxi tribe. It is said that on quiet nights you can still hear them singing their death chant.
In terms of aquatic life, the Congo River Basin has a very high species richness and among the highest known densities of endemics. As of 2009, almost 800 fish species have been recorded from the Congo River Basin (not counting Lake Tanganyika, which is connected but ecologically very different), and large sections remain virtually unstudied. For example, the section in Salonga National Park, which is about the size of Belgium, had still not been sampled at all in 2006. New fish species are scientifically described with some regularity from the Congo River Basin, and many undescribed species are known.
Lower Congo constitutes the ‘lower’ parts of the great river; that is the section of the river from the river mouth at the Atlantic coast to the twin capitals of Brazzaville and Kinshasa. In this section of the river, there are two significant tributaries, both on the left or south side. The Kwilu River originates in the hills near the Angolan border and enters the Congo some 100 km upstream from Matadi. The other being the Inkisi River, that flows in a northerly direction from the Uíge Province in Angola to the confluence with the Congo at Zongo some 80 km downstream from the twin capitals. Because of the vast number of rapids, in particular the Livingstone Falls, this section of the river is not operated continuously by riverboats.The party left Nyangwe overland through the dense Matimba forest. On November 19 they reached the Lualaba again. Since the going through the forest was so heavy, Tippu Tip turned around with his party on December 28, leaving Stanley on his own, with 143 people, including eight children and 16 women. They had 23 canoes. His first encounter with a local tribe was with the cannibal Wenya. In total Stanley reports 32 unfriendly meetings on the river, some violent, even though he attempted to negotiate a peaceful thoroughfare. But the tribes were wary as their only experience of outsiders was with slave traders.
How deep is the Mississippi river right now?
Summary: Depth Of Mississippi RiverAverage Depth9-12 ftDeepest point200 ft30 May 2023
The Europeans had not reached the central regions of the Congo basin from either the east or west, until Henry Morton Stanley’s expedition of 1876–77. At the time one of the last open questions of the European exploration of Africa was whether the Lualaba River fed the Nile (Livingstone’s theory), the Congo or even the Niger River. Financed in 1874, Stanley’s first trans-Africa exploration started in Zanzibar and reached the Lualaba on October 17, 1876. Overland he reached Nyangwe, the center of a lawless area containing cannibal tribes at which Tippu Tip based his trade in slaves. Stanley managed to hire a force from Tippu Tip to guard him for the next 150 kilometres (90 mi) or so, for 90 days.On August 3 they reached the hamlet Nsada. From there Stanley sent four men with letters forward to Boma, asking for food for his starving people. On August 7 relief came, being sent by representatives from the Liverpool trading firm Hatton & Cookson. On August 9 they reached Boma, 1,001 days since leaving Zanzibar on November 12, 1874. The party then consisted of 108 people, including three children born during the trip. Most probably (Stanley’s own publications give inconsistent figures), he lost 132 people through disease, hunger, drowning, killing and desertion.
From this point, the tribes were no longer cannibals but possessed firearms, apparently as a result of Portuguese influence. Some four weeks and 1,900 kilometres (1,200 mi) later he reached Stanley Pool (now Pool Malebo), the site of the present day cities Kinshasa and Brazzaville. Further downstream were the Livingstone Falls, misnamed as Livingstone had never been on the Congo: a series of 32 falls and rapids with an elevation change of 270 metres (900 ft) over 350 kilometres (220 mi). On 15 March they started the descent of the falls, which took five months and cost numerous lives. From the Isangile Falls, five falls from the foot, they beached the canoes and Lady Alice and left the river, aiming for the Portuguese outpost of Boma via land.
In February 2005, South Africa’s state-owned power company, Eskom, announced a proposal to expand generation through improvements and the construction of a new hydroelectric dam. The project would bring the maximum output of the facility to 40 gigawatts (54,000,000 hp). It is feared that these new hydroelectric dams could lead to the extinction of many of the fish species that are native to the river. The Congo River (Kongo: Nzâdi Kôngo, French: Fleuve Congo, Portuguese: Rio Congo), formerly also known as the Zaire River, is the second-longest river in Africa, shorter only than the Nile, as well as the third largest river in the world by discharge volume, following the Amazon and the Ganges rivers. It is also the world’s deepest recorded river, with measured depths of around 219.5 m (720 ft). The Congo-Lualaba-Chambeshi River system has an overall length of 4,700 km (2,920 mi), which makes it the world’s ninth-longest river. The Chambeshi is a tributary of the Lualaba River, and Lualaba is the name of the Congo River upstream of Boyoma Falls, extending for 1,800 km (1,120 mi). The Congo has by far the highest diversity of any African river system; in comparison, the next richest are the Niger, Volta and Nile with about 240, 140 and 130 fish species, respectively. Because of the great ecological differences between the regions in the Congo basin —including habitats such as river rapids, deep rivers, swamps, and lakes— it is often divided into multiple ecoregions (instead of treating it as a single ecoregion). Among these ecoregions, the Livingstone Falls cataracts has more than 300 fish species, including approximately 80 endemics while the southwestern part (Kasai River basin) has more than 200 fish species, of which about a quarter are endemic.The Congo’s drainage basin covers 4,014,500 km (1,550,000 sq mi), an area nearly equal to that of the European Union. The Congo’s discharge at its mouth ranges from 23,000 to 75,000 m/s (810,000 to 2,650,000 cu ft/s), with an average of 41,000 m/s (1,400,000 cu ft/s). The river transports annually 86 million tonnes of suspended sediment to the Atlantic Ocean and an additional 6% of bedload.
Although the Livingstone Falls prevent access from the sea, nearly the entire Congo above them is readily navigable in sections, especially between Kinshasa and Kisangani. Large river steamers worked the river until quite recently. The Congo River still is a lifeline in a land with few roads or railways. Railways now bypass the three major falls, and much of the trade of Central Africa passes along the river, including copper, palm oil (as kernels), sugar, coffee, and cotton.
Several species of turtles and the slender-snouted, Nile and dwarf crocodile are native to the Congo River Basin. African manatees inhabit the lower parts of the river.
The entire Congo basin is populated by Bantu peoples, divided into several hundred ethnic groups. Bantu expansion is estimated to have reached the middle Congo by about 500 BC and the upper Congo by the first century AD. Remnants of the aboriginal population displaced by the Bantu migration, Pygmies/Abatwa of the Ubangian phylum, remain in the remote forest areas of the Congo Basin.
The dominant fish families – at least in parts of the river – are Cyprinidae (carp/cyprinids, such as Labeo simpsoni), Mormyridae (elephant fishes), Alestidae (African tetras), Mochokidae (squeaker catfishes), and Cichlidae (cichlids). Among the natives in the river is the huge, highly carnivorous giant tigerfish. Three of the more unusual endemics are the whitish (non-pigmented) and blind Lamprologus lethops, which is believed to live as deep as 160 metres (520 ft) below the surface, Heterochromis multidens, which is more closely related to cichlids of the Americas than other African cichlids, and Caecobarbus geertsii, the only known cavefish in Central Africa. There are also numerous endemic frogs and snails. Several hydroelectric dams are planned on the river, and these may lead to the extinction of many of the endemics.
Is the Mississippi river level rising?
Levels are rising now but to a point where it may introduce other complicating factors. Water levels along the Mississippi River near Memphis are more than 21 feet, which is nearly a foot higher than where they were in April 2023, according to the U.S. Geological Survey.
The name Congo/Kongo originates from the Kingdom of Kongo once located on the southern bank of the river. The kingdom in turn was named for the indigenous Bantu Kongo people, known in the 17th century as “Esikongo”. South of the Kingdom of Kongo proper lay the similarly named Kakongo kingdom, mentioned in 1535. Abraham Ortelius labeled “Manicongo” as the city at the mouth of the river in his world map of 1564. The tribal names in Kongo possibly derive from a word for a public gathering or tribal assembly. The modern name of the Kongo people or Bakongo was introduced in the early 20th century.Measured along with the Lualaba, the main tributary, the Congo River has a total length of 4,370 km (2,715 mi). It is the only major river to cross the Equator twice. The Congo Basin has a total area of about 4,000,000 km (1,500,000 sq mi), or 13% of the entire African landmass.
The upper Congo basin runs west of the Albertine Rift. Its connection to the Congo was unknown until 1877. The extreme northeast of the Congo basin was reached by the Nilotic expansion at some point between the 15th and 18th centuries, by the ancestors of the Southern Luo speaking Alur people. Francisco de Lacerda followed the Zambezi and reached the uppermost part of the Congo basin (the Kazembe in the upper Luapula basin) in 1796.The Congo’s formation may have led to the allopatric speciation of the bonobo and the common chimpanzee from their most recent common ancestor. The bonobo is endemic to the humid forests in the region, as are other iconic species like the Allen’s swamp monkey, dryas monkey, aquatic genet, okapi, and Congo peafowl.
The Congo basin covers ten countries and accounts for about 13% of Africa. The highest point in the Congo basin is in the Ruwenzori Mountains, at an altitude of around 4,340 m above sea level.
The Congo River is the most powerful river in Africa. During the rainy season over 50,000 cubic metres (1,800,000 cu ft) of water per second flows into the Atlantic Ocean. Opportunities for the Congo River and its tributaries to generate hydropower are therefore enormous. Scientists have calculated that the entire Congo Basin accounts for 13 percent of global hydropower potential. This would provide sufficient power for all of Sub-Saharan Africa’s electricity needs.
On January 6, 1877, after 640 kilometres (400 mi), they reached Boyoma Falls (called Stanley Falls for some time after), consisting of seven cataracts spanning 100 kilometres (60 mi) which they had to bypass overland. It took them to February 7 to reach the end of the falls. Here Stanley learned that the river was called Ikuta Yacongo, proving to him that he had reached the Congo and that the Lualaba did not feed the Nile.
Is it safe to swim in the Mississippi River?
“There can be debris that may not be there. It can change from day to day.” Dugan says she would “absolutely” swim in the Mississippi, but swimmers are encouraged to always wear a life jacket – even in knee-high water – and to shower afterward.
Currently, there are about 40 hydropower plants in the Congo Basin. The largest are the Inga dams, about 200 kilometres (120 mi) southwest of Kinshasa. The project was launched in the early 1970s, when the first dam was completed. The plan (as originally conceived) called for the construction of five dams that would have had a total generating capacity of 34,500 megawatts (MW). To date only the Inga I and Inga II dams have been built, generating 1,776 MW.
Kinshasa was founded as a trading post by Stanley in 1881 and named Léopoldville in honor of Leopold II of Belgium. The Congo Basin was privately claimed by Leopold II as Congo Free State in 1885 where the many Atrocities in the Congo Free State were committed until the region was called the Belgian Congo.
The current course of the Congo River formed between 1.5 and 2 million years BP, during the Pleistocene. It is likely that during this period many upper tributaries of the Congo were captured from adjacent river basins, including the Uele and upper Ubangi from the Chari system and the Chambeshi River alongside a number of upper Kasai River tributaries from the Zambezi system.
What is the current Mississippi River stage?
River StagesLocationRiverCurrentCape GirardeauMississippi River9.98 ft.ChesterMississippi River4.34 ft.ThebesMississippi River9.22 ft.New MadridMississippi River-0.17 ft.
The Congo flows generally toward the northwest from Kisangani just below the Boyoma Falls, then gradually bends southwestward, passing by Mbandaka, joining with the Ubangi River and running into the Pool Malebo (Stanley Pool). Kinshasa (formerly Léopoldville) and Brazzaville are on opposite sides of the river at the Pool, where the river narrows and falls through a number of cataracts in deep canyons (collectively known as the Livingstone Falls), running by Matadi and Boma, and into the sea at Muanda. The name Zaire is from a Portuguese adaptation of a Kikongo word, nzere (“river”), a truncation of nzadi o nzere (“river swallowing rivers”). The river was known as Zaire during the 16th and 17th centuries; Congo seems to have replaced Zaire gradually in English usage during the 18th century, and Congo is the preferred English name in 19th-century literature, although references to Zahir or Zaire as the name used by the inhabitants remained common. The Democratic Republic of the Congo and the Republic of the Congo are named after it, as was the previous Republic of the Congo which had gained independence in 1960 from the Belgian Congo. The Republic of Zaire during 1971–1997 was also named after the river’s name in French and Portuguese. The river and its tributaries flow through the Congo rainforest, the second largest rainforest area in the world, after the Amazon rainforest in South America. The river also has the second-largest flow in the world, behind the Amazon; the second-largest drainage basin of any river, behind the Amazon; and is one of the deepest rivers in the world, at depths greater than 220 m (720 ft). Because its drainage basin includes areas both north and south of the Equator, its flow is stable, as there is always at least one part of the river experiencing a rainy season.
The sources of the Congo are in the highlands and mountains of the East African Rift, as well as Lake Tanganyika and Lake Mweru, which feed the Lualaba River, which then becomes the Congo below Boyoma Falls. The Chambeshi River in Zambia is generally taken as the source of the Congo in line with the accepted practice worldwide of using the longest tributary, as with the Nile River.
The Kingdom of Kongo was formed in the late 14th century from a merging of the kingdoms of Mpemba Kasi and Mbata Kingdom on the left banks of the lower Congo River. Its territorial control along the river remained limited to what corresponds to the modern Kongo Central province. European exploration of the Congo began in 1482 when Portuguese explorer Diogo Cão discovered the river estuary (likely in August 1482), which he marked by a Padrão, or stone pillar (still existing, but only in fragments) erected on Shark Point. Cão sailed up the river for a short distance, establishing contact with the Kingdom of Kongo. The full course of the river remained unknown throughout the early modern period. The upper Congo River was first reached by the Arab slave trade by the 19th century. Nyangwe was founded as a slavers’ outpost around 1860. David Livingstone was the first European to reach Nyangwe in March 1871. Livingstone proposed to prove that the Lualaba connected to the Nile, but on 15 July, he witnessed a massacre of about 400 Africans by Arab slavers in Nyangwe, which experience left him too horrified and shattered to continue his mission to find the sources of the Nile, so he turned back to Lake Tanganyika. Barges have been able to transport goods down the historically shallow Mississippi only because the US Army Corps of Engineers has been constantly vacuuming the bottom of the river.A four-day break during a cold snap around Christmas gave crews time to do minor maintenance on the vessels. One of the dredges left the district about that time, and the second one left St. Louis last week, Dell’Orco said.
No research has directly linked these drought events to the climate crisis, but scientists are confident that rising temperatures will amplify droughts across much of the US.
He estimated that it cost about $6.5 million to operate two dredges for a month. Throw in a third, and he said the Corps was looking at $10 million a month.Much of the Mississippi River basin is still classified as in a drought, including the lower regions that help farmers transport grain for export, according to the US Drought Monitor.Above-average precipitation across the northern Midwest could help replenish the river throughout the month. That’s when Calhoun and Dell’Orco will be on the lookout for flooding.That could end in the next few weeks, though. Forecasts from the National Weather Service’s Climate Prediction Center offer hope that drought will dissipate in February across much of the Mississippi River basin.It’s unclear how climate change will affect the Mississippi River in the long term, Paul Pastelok, an AccuWeather meteorologist, previously told Insider. But it’s possible that the river’s drought cycle accelerates. Since July, the St. Louis District has dredged about 9 million cubic yards of material from the bottom of the river in about 70 locations, Dell’Orco said. In a normal year, they would dredge only 3 million to 4 million cubic yards. In this case, a summer of record heat waves baked away some of the river’s water, and then a flash drought struck the Ohio and Missouri river valleys, robbing the Mississippi of the snowpack that usually feeds it.”There was a few months of pretty intense management,” Lou Dell’Orco, the chief of operations and readiness at the Corps’ St. Louis District, told Insider.
That’s more than 2,700 Olympic-size swimming pools of material removed from the riverbed this year, compared with just 1,000 Olympic-size swimming pools in a normal season.
“Commerce is moving with no restrictions relative to drought,” Deb Calhoun, a senior vice president at the Waterways Council, a group that advocates for modern waterway infrastructure, told Insider in an email. “We will be watching for high water next, which is something that normally happens around this time of year.”
What does the stage of a river mean?
Stage – the level of the water surface of a river or stream above an established gage datum at a given location.
At some points, three vessels were operating 24/7, traveling to chokepoints in the St. Louis area, dropping their suction tubes to the riverbed, inhaling material from it, and transporting the material through tubes to designated disposal sites — like “a giant vacuum cleaner,” Dell’Orco said.The Mississippi River drought was big news when barges got stranded, receding waters revealed historic artifacts, and river traffic briefly ground to a standstill in October.
JACKSON – Continued heavy rainfall and projected Pascagoula River levels have resulted in extensive flooding of Pascagoula River Wildlife Management Area (WMA). Effective December 29, 2018, Pascagoula River (WMA) will be closed to public access except for waterfowl hunting to river gauge levels. All deer and small game hunting is closed based on these parameters:
What is the deepest river in the world?
The Congo-Lualaba-Chambeshi It is also the world’s deepest recorded river, with measured depths of around 219.5 m (720 ft). The Congo-Lualaba-Chambeshi River system has an overall length of 4,700 km (2,920 mi), which makes it the world’s ninth-longest river.
The river is expected to rise to 17.3 feet this morning. At 16 feet, river property in the Cumbest Bluff area will be cutoff and some river roads will be impassable.
With additional rainfall received Wednesday, the river is expected to remain at this level for several days, dropping to 16.5 feet on Monday afternoon.
Heather Brown loves to put her curiosity to work to answer your Good Questions on WCCO 4 News at 10, and helps you kick your weekdays off on WCCO This Morning and WCCO Mid-Morning.South of St. Cloud, the average E. coli level does violate the state standard. But Friends of the Mississippi says that doesn’t mean you can’t swim here.
MINNEAPOLIS – Minnesotans seem to have no problem jumping in and splashing around the state’s 10,000 lakes, but what about one of Minnesota’s crown jewels: the Mississippi River?Friends of the Mississippi published a “State of the River” report MPCA data, measuring the phosphorus, nitrate and sediment that can harm the fish, bugs and plants. The chemicals won’t hurt people, but bacteria like E. coli could.
“It’s not like a pool where you can see a kid swimming in the water. Of course, it’s moving water, so there’s faster water, there can be currents,” Dugan said. “There can be debris that may not be there. It can change from day to day.”
Even though homes aren’t expected to flood in that area, emergency officials are keeping a close watch and warning residents in low-lying areas to evacuate ahead of the Pearl River cresting because roads may be underwater. “There are a few roads and parks that might have some water on them,” he said. “We tend to not see water getting into homes until closer to 30-30⅟₂ feet.” The development in the northwest Caribbean is the one to watch, Winesett said, although the National Hurricane Center predicts a roughly 20% chance of developing in the next five days.
“We’re trying to get messages out to residents to prepare,” Brown said. “While there are no mandatory evacuations, people need to get their personal evacuation kits together and be prepared that their homes can be inaccessible for days.”
“We’re looking at cresting overnight, which makes it particularly dangerous for folks if they wait until the last minute to evacuate,” said John Brown, spokesman for the American Red Cross in Jackson.”It doesn’t look very impressive right now,” Winesett said. “If anything develops with that wave, it would probably stay west of us. With that being said, there could be some tropical moisture returning back to the area by Labor Day weekend. We’re still about a week out, so it’s something we’re keeping an eye on.”
Many of the areas where the rivers are at or above flood stage remain under a flood warning into early September. Some areas will remain under a flood warning until further notice, weather service officials reported.
∎ At Monticello rose above the 22-foot flood stage on Thursday. As of Sunday, the river was at 26 feet. The Pearl is expected to crest at 28 feet on Wednesday.At the same time, forecasters with the National Hurricane Center are keeping watch over four tropical developments in the Atlantic arena, including one in the northwest Caribbean Sea. One, in the Atlantic Ocean, has a 70% possibility of developing into a tropical depression or a named storm in the next five days.
There have been three named storms so far this year in 2022. The most recent was Tropical Storm Colin, which developed off the Carolinas’ coast during the Fourth of July weekend.
Do you have a story to share? Contact Lici Beveridge at [email protected]. Follow her on Twitter @licibev or Facebook at facebook.com/licibeveridge.
∎ Near Carthage reached flood stage of 17 feet on Wednesday and crested at nearly 24 feet Thursday. The river remained above flood stage Sunday afternoon at 21⅟₂ but is expected to return to below flood level by Tuesday evening.
The Pearl River is expected to crest sooner and lower than expected in the Jackson area, below the 26-foot barrier that would indicate widespread local damage.
∎ At Bovina was at 35 feet Sunday afternoon — 7 feet above flood stage of 28 feet. It is expected to crest at 37⅟₂ feet Monday afternoon and remain at that level into Tuesday evening.
“Monticello can be in the crosshairs, but we have seen some positives signs with the water release (at Ross Barnett Reservoir) and how the weather is cooperating somewhat — we don’t think it will contribute to additional flooding,” Brown said.
“There will be some flooding impact on the Pearl downstream,” Winesett said. “There’s going to be a lot of agricultural and low-lying land getting impacted.”Some areas of Mississippi can still expect flooding, particularly along the Pearl, Big Black and Pascagoula rivers, even though the bulk of the heavy rains that have plagued the state for the last week has subsided.
Monticello, to the south of Jackson, is one of the areas that is expected to crest well above flood stage, but is not expected to cause flooding to homes and other structures, Winesett said. The river should crest around 28 feet mid week.Thomas Winesett, a meteorologist with the National Weather Service in Jackson, said although the Pearl and other rivers in Mississippi are expected to crest above flood stage, little to no impact to homes and other structures is expected.
What is the Pascagoula River stage at Merrill?
Flood stage ranges from 22.00 ft to a gauge height of 32.00 ft for major flooding events.
Click on the links below to obtain today’s forecast for that location. Claiborne L&D Alabama -CLBA1 Weiss Dam Coosa -CREA1. Coffeeville L&D Tailwater Tombigbee -CLDA1. Pascagoula River Basin.
Free Flowin’ on the Riverfront V T RFree Flowin’ on the Riverfront is a music festival to celebrate the beauty of the Pascagoula IVER U.S. freeflowin.netMedical Assistant Programs Pascagoula River Estates, MS – CMAPrograms.org – Find Medical Assistant Training Near You! Interested in medical assistant programs in Pascagoula River j h f Estates, MS? See our full data base of professional CMA schools and locate the ideal program for you! Pascagoula, MS Severe Weather Alert | Weather Underground Get the weather forecast with today, tomorrow, and 10-day forecast graph. Doppler radar and rain conditions from Weather Underground. D @Medical Care for the MS Gulf Coast | Singing River Health System Providing award-winning medical care for patients throughout their lives at our hospitals, clinics, and specialty centers as well as hospice services.Minor Flooding is defined to have minimal or no property damage, but possibly some public threat. A FLOOD ADVISORY product is issued to advise the public of flood events that are expected not to exceed the minor flood category. Examples of conditions that would be considered minor flooding include: The purpose of this document is to explain the terminology used by the National Weather Service related to high water levels on streams and lakes in Alaska. There are uncountable numbers of streams and lakes of various sizes in Alaska and only a very small fraction of these have gages that monitor the water levels. Gages are devices that allow for the manual or automated monitoring of water level. The term used for the water level of a stream or lake at a gage is stage. Moderate Flooding is defined to have some inundation of structures and roads near the stream. Some evacuations of people and/or transfer of property to higher elevations may be necessary. A FLOOD WARNING should be issued if moderate flooding is expected during the event. Examples of conditions that would be considered moderate flooding include:High water terms used by the National Weather Service include bankfull stage, action stage, and flood stage as defined below. In Alaska, the sparse gage network requires that these terms be defined with a broader definition that reflects characteristics of the gaged waterbody and well as nearby waterbodies. Thus the definitions consider both the specific impacts that can be documented in the vicinity of the gage as well as the expected impacts that could result on any waterbody in the general area during an event of that magnitude. The assignment of these stages thus includes the combined assessment of specific impacts and the frequency of occurrence of the event. The concept of using the frequency of occurrence of high water events to supplement the assessment of flood stages is based on the assumption that frequently occurring water levels such as the 2-year flood (50% chance of occurring in any year) will have few impacts in comparison to the significant impacts expected during an infrequent event such as a 100-year flood (1% chance of occurring in any year). When high water stages are determined from a flood frequency analysis, the impacts listed for the applicable stages will be the recurrence interval associated with that level and a qualifier to assess the quality of the recurrence interval estimate.
Stage – the level of the water surface of a river or stream above an established gage datum at a given location. The gage datum is a horizontal surface used as a zero point for measurement of water level. This gage datum level usually is located slightly below the lowest point of the stream bottom such that the stage is greater than the maximum depth of water.
Flood Stage – an established gage height for a given location above which a rise in water surface level begins to create a hazard to lives, property, or commerce. The issuance of flood advisories or warnings is linked to flood stage. Not necessarily the same as bankfull stage.
In remote areas with few specific impacts, floods with 50-100 year recurrence interval would be assumed to be causing major flooding on streams in the area.
In remote areas with few specific impacts, floods with 5-10 year recurrence interval would be assumed to be causing minor flooding on streams in the area.Major Flooding is defined to have extensive inundation of structures and roads. Significant evacuations of people and/or transfer of property to higher elevations are necessary. A FLOOD WARNING should be issued if major flooding is expected during the event. Examples of conditions that would be considered major flooding include:In remote areas with few specific impacts, floods with 15-40 year recurrence interval would be assumed to be causing moderate flooding on streams in the area.
Since gages are sparse in Alaska, the stage measured at each gage is used as an index of water level characteristics upstream and downstream of the gage in addition to the status at the gage. In many cases, there is only one gage on a stream system and thus the gage represents the water level characteristics in the entire stream basin. The gage is also often used to indicate the water level status of other streams or lakes in the general area that have similar characteristics to the gaged stream. People living or recreating near any stream or lake should identify the closest gage that can be used as an index for the expected water level changes at their location. Bankfull Stage – an established gage height at a given location along a river or stream, above which a rise in water surface will cause the river or stream to overflow the lowest natural stream bank somewhere in the corresponding reach. The term “lowest bank” is however, not intended to apply to an unusually low place or a break in the natural bank through which the water inundates a small area. Bankfull stages on streams with natural or manmade high banks can be defined by the predominant vegetation line on the banks. The bankfull stage on many streams is associated with the 2-year recurrence interval flood. Bankfull stage is not necessarily the same as flood stage. Flood categories are terms defined for each gage location that describe or categorize the observed or expected severity of flood impacts in the corresponding stream segment or nearby stream. The severity of flooding at a given stage is not necessarily the same at all locations along a stream due to varying channel/bank characteristics on portions of the stream. Therefore, the stage for a given flood category is usually associated with lowest water level corresponding to the most significant flood impacts somewhere in the reach. The flood categories used in the NWS are minor, moderate, and major flooding, but all three of the flood categories do not necessarily exist for each gage location. Most commonly, gages in remote areas may not have a major flood stage assigned. Record flooding is flooding that equals or exceeds the highest stage or discharge at a given site during the period of record keeping.Action Stage – the stage which, when reached by a rising stream, represents the level where the NWS or a partner/user needs to take some type of mitigation action in preparation for possible significant hydrologic activity. The type of action taken varies for each gage location. Gage data should be closely monitored by any affected people if the stage is above action stage.A 30 percent chance of showers and thunderstorms, mainly after 5pm. Mostly sunny and hot, with a high near 95. Calm wind becoming southwest around 5 mph in the afternoon.A 40 percent chance of showers and thunderstorms, mainly after 2pm. Mostly sunny, with a high near 93. Calm wind becoming south around 5 mph in the afternoon.
A 30 percent chance of showers and thunderstorms, mainly before 8pm. Partly cloudy, with a low around 76. South wind around 5 mph becoming calm in the evening.
A 20 percent chance of showers and thunderstorms after noon. Sunny and hot, with a high near 98. Heat index values as high as 109. Calm wind becoming west around 5 mph in the morning.
Is the Mississippi River still drying up?
The Mississippi River is currently going through a historic drought, with multiple parts experiencing record-low water levels. On top of that, riverbeds are drying up one by one under the eyes of more than 20 million people who use daily drinking water supplied with the help of the Mississippi River.
A 40 percent chance of showers and thunderstorms, mainly before 8pm. Mostly cloudy, with a low around 76. South wind around 5 mph becoming calm in the evening.
Bankfull Stage – an established gauge height at a given location along a river or stream, above which a rise in water surface will cause the river or stream to overflow the lowest natural stream bank somewhere in the corresponding reach. The term “lowest bank” is however, not intended to apply to an unusually low place or a break in the natural bank through which the water inundates a small area. Bankfull stages on streams with natural or manmade high banks can be defined by the predominant vegetation line on the banks. The bankfull stage on many streams is associated with the 2-year recurrence interval flood. Bankfull stage is not necessarily the same as flood stage.
Therefore, the stage for a given flood category is usually associated with lowest water level corresponding to the most significant flood impacts somewhere in the reach. The flood categories used in the NWS are minor, moderate, and major flooding, but all three of the flood categories do not necessarily exist for each gage location. Most commonly, gages in remote areas may not have a major flood stage assigned.Since gauges are sparse in Alaska, the stage measured at each gauge is used as an index of water level characteristics upstream and downstream of the gauge in addition to the status at the gauge. In many cases, there is only one gauge on a stream system and thus the gauge represents the water level characteristics in the entire stream basin.
Is the Mississippi River still in drought stage?
Much of the Mississippi River basin is still classified as in a drought, including the lower regions that help farmers transport grain for export, according to the US Drought Monitor.
The assignment of these stages thus includes the combined assessment of specific impacts and the frequency of occurrence of the event. The concept of using the frequency of occurrence of high water events to supplement the assessment of flood stages is based on the assumption that frequently occurring water levels such as the 2-year flood (50% chance of occurring in any year) will have few impacts in comparison to the significant impacts expected during an infrequent event such as a 100-year flood (1% chance of occurring in any year).Gauges are devices that allow for the manual or automated monitoring of water level. The term used for the water level of a stream or lake at a gauge is stage.
The purpose of this document is to explain the terminology used by the National Weather Service related to high water levels on streams and lakes in Alaska. There are uncountable numbers of streams and lakes of various sizes in Alaska and only a very small fraction of these have gauges that monitor the water levels.
The gauge is also often used to indicate the water level status of other streams or lakes in the general area that have similar characteristics to the gauged stream. People living or recreating near any stream or lake should identify the closest gauge that can be used as an index for the expected water level changes at their location.When high water stages are determined from a flood frequency analysis, the impacts listed for the applicable stages will be the recurrence interval associated with that level and a qualifier to assess the quality of the recurrence interval estimate.