1
To learn more, check out these Web sites: www.glerl.noaa.gov/ www.oar.noaa.gov/ www.glerl.noaa.gov/seagrant/ glwlphotos/Seiche/ Your Erie Times-News has important information about the weather and Lake Erie marine conditions every day. Find the following: The temperature for the day, amount of precipitation, wind speed, waves, water temperature and lake level. Keep track of these for a week and then plot them on a graph. What: Visiting scientist lecture, “The Coyotes of Presque Isle,” by Tracy Graziano When: Tonight at 7 p.m. Where: The Tom Ridge Environmental Center For more information, contact: Jeanette Schnars at 835-6975 or visit www.RegSciConsort.com What: Presque Isle After Dark program, “Night walk at Erie Bluffs State Park” When: Saturday, Jan. 31, 6 to 8 p.m. If you are not sure how to get to the Bluffs, meet the naturalist at the Tom Ridge Environmental Center; departure is at 5:30 p.m. Bring a flashlight. Dress appropriately for the outdoors. The walk will be about one mile long. Fore more information, contact: Brian Gula, environmental education specialist, 217-9632 What: Presque Isle Little Naturalist program, “Critters under cover,” for children ages 3 to 6 accompanied by an adult. Be prepared to be outdoors for the full hour. When: Wednesday, Feb.4, from 1 to 2 p.m. Where: Meet at the Rotary Pavilion to explore Presque Isle forests and discover the critters that hide under logs and in other habitats. After the program, join us for hot cocoa at the Ranger Station and warm up by the fire. No fee. No registration required. For more information, contact: Emily Borcz, environmental education specialist, 838-2454 What: Family fishing at Presque Isle State Park, sponsored by the Pennsylvania Department of Conservation and Natural Resources, the Pennsylvania Fish and Boat Commission and the SONS of Lake Erie. Where: The Rotary Pavilion at the East Pond, When: Saturday, Feb. 14, from 11 a.m. to 3 p.m.The SONS will be cooking up hot dogs. All equipment is provided. No fee. No registration. Appropriate for all ages. Dress appropriately for the outdoors. No ice that day, no problem.We will still fish in Waterworks Pond with regular gear. For more information, contact: Brian Gula, environmental education specialist, 217-9632 What: Build your own pair of traditional wooden snowshoes Where: Tom Ridge Environmental Center. When: Saturday, Feb. 21, from 9 a.m. to 3 p.m. Cost: for the workshop is $155. Fee includes instruction, adjustable bindings, ash wood frames, nylon lacing, and lunch — everything you need to complete your very own pair of quality snowshoes with confidence and ease. Registration and payment is due by Feb. 1 to ensure that your kit arrives in time for the workshop. For more information, contact: Kathleen Ryan, environmental education specialist, 833-0793 to register. LEARN MORE 14 hours The period of a typical seiche across Lake Erie. For other lakes, the period is shorter, for example, in Lake Champlain in upstate New York, it’s four hours;Scotland’s Loch Ness, about 30 minutes. 06/26/1954 A seiche 2.44 meters (8 feet) high and 40 km (25 miles) wide hit Chicago’s lakefront. Eight people were killed, most of whom were swept into the water and drowned while fishing in Montrose Harbor. 1890 The year the term seiche was first promoted by the Swiss hydrologist François-Alphonse Forel who had observed the effect in Lake Geneva, Switzerland.The word originates in a Swiss French dialect word that means “to sway back and forth.” SOURCE: www.fact-archive.com/encyclopedia/Seiche BY THE NUMBERS CONTRIBUTED PHOTO On Dec. 28, the power of waves fueled by steady winds broke up the ice dunes that were protecting the shoreline and created conditions for a seiche in Buffalo. Similar conditions on Jan. 30, 2008, caused high water level and waves of 12 to 16 feet, resulting in a record seiche that caused flooding in Buffalo. Theword“seiche”(pronounced saysh) may have no meaning for you. But people who have experi- enced the phenomena know that it can cause death and destruc- tion in moments. One of the greatest disasters in Buffalo was caused by a seiche. It was produced by prolonged strong winds pushing the water toward that end of Lake Erie. It occurred at 11 p.m. on Oct. 18, 1844, when a wall of water 22 feet high quickly inundated the com- mercial and residential districts along the waterfront. Without warning, the water breached the 14-foot sea wall and flooded the waterfront. Seventy-eight people drowned that day, according to newspaper accounts. When the winds stopped, the water moved back in the direction from which it came. A seiche occurs in an enclosed body of water such as a lake, bay or gulf. Like water sloshing back and forth in a bath tub, the water in the lake is pushed by strong winds and rapid changes in at- mospheric pressure, causing the water level to rise on one side of the lake as it goes down on the op- posite side. The waves slosh back and forth between shores of the lake basin and with no warning, cause huge fluctuations where the shoreline and harbor water levels can rise or fall by many feet. Most seiches go unnoticed and never cause much damage in the Great Lakes because they are rel- atively subtle and imperceptible, causing water levels on beaches to rise just a foot or less. However, because Lake Erie is the shallowest of the Great Lakes, the effects of storm-driven waves are amplified and when the wind blows from the southwest to the northeast, seiches are more dra- matic. Another record seiche in Buf- falo happened on Jan. 30, 2008. Sustained strong winds following the passage of a cold front caused the Lake Erie water level to rise substantially. The high water lev- els and waves of 12 to 16 feet re- sulted in erosion of the lake shore and significant flooding at the ex- treme eastern end of the lake. Roads along the lake shore were water-covered or closed be- cause of spray. Floodwaters inun- dated the First Ward (west side) of the city of Buffalo, with entire neighborhoods under water. The Lake Erie water level rose 11 feet above its eight-foot flood stage for over three hours. According to the National Oceanic and Atmo- spheric Administration, this was the second highest lake level on record. That same day in Erie, the southwest winds blew steady at 35 mph and gusted up to 54 mph throughout the day. As the water was pushed to the northeast, the high water combined with 12-foot waves and caused flooding on the peninsula and lifted docks from their moorings. Harry Les- lie, park operations manager at Presque Isle State Park, said: “Presque Isle Bay filled up with five to six feet of water from one of the strongest storms I had wit- nessed since I started working at the park in 1989.” The power unleashed by the waves and high water toppled ice dunes that had formed on the lake side and broke up the ice on the bay, which had been dotted with anglers before the storm. “One day you saw people ice fish- ing; the next day you could take a boat out,” Leslie said. A similar storm occurred on Dec. 28 after a record-high tem- perature of 67. The cold front that whipped across the area that morning brought damaging winds and created the right conditions for another seiche. Winds, as high as 75 mph, wreaked havoc with the Buffalo Bills game and resulted in power outages to thousands. Three duck hunters were rescued from the Barcelona Harbor when their duck boats were swamped by high winds, rain and waves. A sec- tion of Route 5 was closed near Hamburg, N.Y., but fortunately this time the water level in Buf- falo did not reach a record high. The wicked winds that wreak havoc and cause seiches when they whip across the waters of Lake Erie ended 2008 much as they began — stirring up waves that rip out sections of beach, cause flooding and trigger dra- matic rescues. ANNA McCARTNEY , Newspaper in Education coordinator, can be reached by e-mail. Can you say ‘seiche?’ Weather phenomenon creates dramatic effect on Lake Erie By ANNA McCARTNEY [email protected] Lake Erie is the shallowest of the Great Lakes, reaching a max- imum depth of 210 feet in the eastern basin. The axis of Lake Erie runs from southwest to northeast, corresponding to the direction of prevailing winds. Lake topography combined with changing water levels and strong waves can have extreme effects on the shoreline. Because of the lake’s shallow- ness and elongation, strong winds can push water toward one end of Lake Erie (setup), causing some of the most extreme lake setups observed in the world. A differ- ence in elevation of over 15 feet or more between the ends of the lake can occur. When the wind stops, the water rebounds. This seiche effect can cause the water to move back and forth across the lake for some time. When seiches of two feet or greater are likely to occur, the National Weather Service is- sues advisories for portions of the Great Lakes. These rises in water levels can provide a base on which high waves can attack the upper part of a beach and penetrate farther inland. Wind- induced surges accompanied by wave action account for most of the damage to coastal structures and beach areas. The four factors that influ- ence the formation of waves caused by wind and that deter- mine wave size are: water that the wind has blown over. over a given area. The greater each of the above factors, the larger the waves. Waves are characterized by: trough to crest). crest to crest). arrival of consecutive crests at a stationary point). - agation or ways in which they travel. Waves in a given area typi- cally have a range of heights. For weather reporting and for scientific analysis of wind wave statistics, their characteristic height over a period of time is usually expressed as significant wave height. This figure repre- sents an average height of the highest one-third of the waves in a given time period (usually in the range from 20 minutes until 12 hours), or in a specific wave or storm system. Because the wave height var- ies, the largest individual waves are likely to be about twice the reported significant wave height for a particular day or storm. ANNA McCARTNEY , Newspaper in Education coordinator, can be reached by e-mail. Wind-driven waves can damage shorelines By ANNA McCARTNEY [email protected] CONTRIBUTED PHOTO Because Lake Erie is the shallowest of the Great Lakes, the effects of storm-driven waves are amplified. The high water levels and waves cause erosion of the lake shore and significant flooding. Physical processes have a ma- jor impact on environmental, chemical, and biological pro- cesses and influence many oth- er types of user activities. Water supply management, waste wa- ter management, power plant sit- ings, shipping, recreational and commercial boating and fishing, shoreline erosion and redistri- bution of sedimentary material all rely on good forecasts. NOAA’s Great Lakes Environ- mental Research Laboratory (GLERL) has a long history of addressing a wide range of en- vironmental issues in the Great Lakes and other coastal envi- ronments. GLERL is the only NOAA research laboratory that has the breadth of scientific ex- pertise to address complex Great Lakes ecosystem issues. GLERL research and programs provide important information to deci- sion-makers and others to help them make good choices. All of GLERL’s long-range re- search is targeted toward pro- ducing a suite of forecasts and forecasting capabilities of physi- cal and ecological conditions that will advance an ecosystem-based approach to management. The Great Lakes Coastal Fore- cast System, the GLCFS Web site, (www.glerl.noaa.gov/res/glcfs/) is a useful forecasting system for all users of the Great Lakes coastal waters who require real- time information and forecasts of temperatures, currents, water levels, and waves. These forecasts provide Na- tional Weather Service marine forecasters with a significant source of information, which should lead to considerable im- provements both in the accuracy and efficiency of marine fore- casts for the Great Lakes. GLERL also has exceptional resources for teachers to make Great Lakes data more acces- sible and easy to use with their students. Great Lakes Water Data Sets for Teachers (http://people. emich.edu/srutherf/NOAA/) con- tains real data extracted from on-going and historic GLERL research projects, including temperature, dissolved oxygen and seiche data. Data is in a format that is easy to use in the classroom. Middle or high school students and teachers can conduct their own inquiries, support guided inqui- ries, demonstrate limnological concepts or just practice graph- ing, mapping and mathematics using real data. ANNA McCARTNEY , Newspaper in Education coordinator, can be reached by e-mail. Where to find marine forecasts, data, more CONTRIBUTED GRAPHIC Wind set-up is a local rise in water caused by winds pushing water to one side of the lake. An extreme form of oscillation known as a seiche occurs when there are rapid changes in winds and barometric pressure. This diagram is from www.epa.gov/glnpo/atlas/glat- ch3.html. By ANNA McCARTNEY [email protected] Tuesday, January 13, 2009 | Erie Times-News | GoErie.com | 3D

CONTRIBUTED PHOTO Can you say ‘seiche?’

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Page 1: CONTRIBUTED PHOTO Can you say ‘seiche?’

To learn more, checkout these Web sites:

www.glerl.noaa.gov/www.oar.noaa.gov/www.glerl.noaa.gov/seagrant/

glwlphotos/Seiche/

Your Erie Times-News hasimportant information about theweather and Lake Erie marineconditions every day. Findthe following: Thetemperature for theday, amount ofprecipitation, windspeed, waves, watertemperature and lakelevel. Keep track of thesefor a week and then plotthem on a graph.

What: Visiting scientist lecture, “The Coyotes of Presque Isle,” byTracy GrazianoWhen: Tonight at 7 p.m.Where: The Tom Ridge Environmental CenterFor more information, contact: Jeanette Schnars at 835-6975 orvisit www.RegSciConsort.com

What: Presque Isle After Dark program, “Night walk at Erie BluffsState Park”When: Saturday, Jan. 31, 6 to 8 p.m. If you are not sure how to get tothe Bluffs, meet the naturalist at the Tom Ridge EnvironmentalCenter; departure is at 5:30 p.m. Bring a flashlight. Dressappropriately for the outdoors. The walk will be about one mile long.Fore more information, contact: Brian Gula, environmentaleducation specialist, 217-9632

What: Presque Isle Little Naturalist program, “Critters under cover,”for children ages 3 to 6 accompanied by an adult. Be prepared to beoutdoors for the full hour.When: Wednesday, Feb. 4, from 1 to 2 p.m.Where: Meet at the Rotary Pavilion to explore Presque Isle forestsand discover the critters that hide under logs and in other habitats.After the program, join us for hot cocoa at the Ranger Station andwarm up by the fire. No fee. No registration required.For more information, contact: Emily Borcz, environmentaleducation specialist, 838-2454

What: Family fishing at Presque Isle State Park, sponsored by thePennsylvania Department of Conservation and Natural Resources,the Pennsylvania Fish and Boat Commission and the SONS of LakeErie.Where: The Rotary Pavilion at the East Pond,When: Saturday, Feb. 14, from 11 a.m. to 3 p.m. The SONS will becooking up hot dogs. All equipment is provided. No fee. Noregistration. Appropriate for all ages. Dress appropriately for theoutdoors. No ice that day, no problem. We will still fish in WaterworksPond with regular gear.For more information, contact: Brian Gula, environmentaleducation specialist, 217-9632

What: Build your own pair of traditional wooden snowshoesWhere: Tom Ridge Environmental Center.When: Saturday, Feb. 21, from 9 a.m. to 3 p.m.Cost: for the workshop is $155. Fee includes instruction, adjustablebindings, ash wood frames, nylon lacing, and lunch — everything youneed to complete your very own pair of quality snowshoes withconfidence and ease. Registration and payment is due by Feb. 1 toensure that your kit arrives in time for the workshop.For more information, contact: Kathleen Ryan, environmentaleducation specialist, 833-0793 to register.

LEARN MORE

14hours

The period of a typical seiche across Lake Erie. For other lakes, theperiod is shorter, for example, in Lake Champlain in upstate New

York, it’s four hours; Scotland’s Loch Ness, about 30 minutes.

06/26/1954A seiche 2.44 meters (8 feet) high and 40 km (25 miles) wide hitChicago’s lakefront. Eight people were killed, most of whom were

swept into the water and drowned while fishing in Montrose Harbor.

1890The year the term seiche was first promoted by the Swiss hydrologist

François-Alphonse Forel who had observed the effect in LakeGeneva, Switzerland. The word originates in a Swiss French

dialect word that means “to sway back and forth.”

SOURCE: www.fact-archive.com/encyclopedia/Seiche

BY THE NUMBERS

CONTRIBUTED PHOTO

On Dec. 28, the power of waves fueled by steady winds broke up the ice dunes that were protecting the shoreline and created conditions for aseiche in Buffalo. Similar conditions on Jan. 30, 2008, caused high water level and waves of 12 to 16 feet, resulting in a record seiche thatcaused flooding in Buffalo.

Theword“seiche”(pronouncedsaysh) may have no meaning foryou.Butpeoplewhohaveexperi-enced the phenomena know thatit can cause death and destruc-tion in moments.

OneofthegreatestdisastersinBuffalo was caused by a seiche.It was produced by prolongedstrong winds pushing the watertoward that end of Lake Erie. Itoccurred at 11 p.m. on Oct. 18,1844,whenawallofwater22feethigh quickly inundated the com-mercial and residential districtsalong the waterfront. Withoutwarning, the water breached the14-foot sea wall and flooded thewaterfront.Seventy-eightpeopledrowned that day, according tonewspaper accounts. When thewinds stopped, the water movedback in the direction from whichit came.

Aseicheoccursinanenclosedbody of water such as a lake, bayor gulf. Like water sloshing backand forth in a bath tub, the waterin the lake is pushed by strongwinds and rapid changes in at-mospheric pressure, causing the

water level to rise on one side ofthelakeasitgoesdownontheop-positeside.Thewavessloshbackand forth between shores of thelake basin and with no warning,cause huge fluctuations wherethe shoreline and harbor waterlevels can rise or fall by manyfeet.

MostseichesgounnoticedandnevercausemuchdamageintheGreatLakesbecausetheyarerel-ativelysubtleandimperceptible,causing water levels on beachesto rise just a foot or less.

However,becauseLakeErieistheshallowestoftheGreatLakes,theeffectsofstorm-drivenwavesareamplifiedandwhenthewindblows from the southwest to thenortheast, seiches are more dra-matic.

Another record seiche in Buf-falo happened on Jan. 30, 2008.Sustainedstrongwindsfollowingthepassageofacoldfrontcausedthe Lake Erie water level to risesubstantially.Thehighwaterlev-els and waves of 12 to 16 feet re-sultedinerosionofthelakeshoreandsignificantfloodingattheex-treme eastern end of the lake.

Roads along the lake shorewerewater-coveredorclosedbe-

causeofspray.Floodwatersinun-dated the First Ward (west side)of the city of Buffalo, with entireneighborhoodsunderwater.TheLakeEriewaterlevelrose11feetaboveitseight-footfloodstageforover three hours. According tothe National Oceanic and Atmo-spheric Administration, this wasthe second highest lake level onrecord.

That same day in Erie, thesouthwest winds blew steady at35 mph and gusted up to 54 mphthroughout the day. As the waterwas pushed to the northeast, thehighwatercombinedwith12-footwaves and caused flooding onthe peninsula and lifted docksfrom their moorings. Harry Les-lie, park operations manager atPresque Isle State Park, said:“Presque Isle Bay filled up withfive to six feet of water from oneof the strongest storms I had wit-nessed since I started working atthe park in 1989.”

The power unleashed by thewaves and high water toppledicedunesthathadformedonthelakesideandbrokeuptheiceonthe bay, which had been dottedwith anglers before the storm.“Onedayyousawpeopleicefish-

ing; thenextdayyoucouldtakeaboat out,” Leslie said.

A similar storm occurred onDec. 28 after a record-high tem-perature of 67. The cold frontthatwhippedacrosstheareathatmorningbroughtdamagingwindsand created the right conditionsfor another seiche.

Winds, as high as 75 mph,wreaked havoc with the BuffaloBillsgameandresultedinpoweroutagestothousands.Threeduckhunters were rescued from theBarcelona Harbor when theirduck boats were swamped byhighwinds,rainandwaves.Asec-tion of Route 5 was closed nearHamburg, N.Y., but fortunatelythis time the water level in Buf-falo did not reach a record high.

The wicked winds that wreakhavoc and cause seiches whenthey whip across the waters ofLake Erie ended 2008 much asthey began — stirring up wavesthat rip out sections of beach,cause flooding and trigger dra-matic rescues.

A N N A M c C A R T N E Y ,Newspaper in Educationcoordinator, can be reached bye-mail.

Can you say ‘seiche?’Weather phenomenon creates dramatic effect on Lake Erie

By ANNA [email protected]

Lake Erie is the shallowest oftheGreatLakes,reachingamax-imum depth of 210 feet in theeastern basin. The axis of LakeErie runs from southwest tonortheast, corresponding to thedirection of prevailing winds.Lake topography combinedwith changing water levels andstrong waves can have extremeeffects on the shoreline.

Because of the lake’s shallow-nessandelongation,strongwindscanpushwatertowardoneendofLake Erie (setup), causing someof the most extreme lake setupsobserved in the world. A differ-ence in elevation of over 15 feetor more between the ends of thelake can occur. When the windstops, the water rebounds. Thisseicheeffectcancausethewatertomovebackandforthacrossthelake for some time.

When seiches of two feet orgreater are likely to occur, theNational Weather Service is-sues advisories for portions ofthe Great Lakes. These rises inwater levels can provide a baseon which high waves can attackthe upper part of a beach andpenetrate farther inland. Wind-inducedsurgesaccompaniedbywave action account for most ofthedamagetocoastalstructuresand beach areas.

The four factors that influ-ence the formation of wavescaused by wind and that deter-mine wave size are:

:7&)< 0+""<-:."2;%*/2%"<&028);"*#*+")

water that the wind has blownover.

:6&(" 2%" 4&)< %80 9'*4)over a given area.

:782"/ <"+2%-The greater each of the above

factors, the larger the waves.Waves are characterized by::783" %"&$%2 ,<&028);" #/*(

trough to crest).:783" '")$2% ,<&028);" #/*(

crest to crest).:5"/&*<,2&("&)2"/38'9"24"")

arrival of consecutive crests at astationary point).

:6%" <&/";2&*) *# 483" +/*+-agation or ways in which theytravel.

Waves in a given area typi-cally have a range of heights.For weather reporting and forscientific analysis of wind wavestatistics, their characteristicheight over a period of time isusually expressed as significantwave height. This figure repre-sents an average height of thehighestone-thirdofthewavesina given time period (usually inthe range from 20 minutes until12 hours), or in a specific waveor storm system.

Because the wave height var-ies, the largest individual wavesare likely to be about twice thereportedsignificantwaveheightfor a particular day or storm.

A N N A M c C A R T N E Y ,Newspaper in Educationcoordinator, can be reached bye-mail.

Wind-driven waves can damage shorelinesBy ANNA [email protected]

CONTRIBUTED PHOTO

Because Lake Erie is the shallowest of the Great Lakes, the effects ofstorm-driven waves are amplified. The high water levels and wavescause erosion of the lake shore and significant flooding.

Physical processes have a ma-jor impact on environmental,chemical, and biological pro-cesses and influence many oth-er types of user activities. Watersupply management, waste wa-termanagement,powerplantsit-ings, shipping, recreational andcommercialboatingandfishing,shoreline erosion and redistri-bution of sedimentary materialall rely on good forecasts.

NOAA’s Great Lakes Environ-mental Research Laboratory(GLERL) has a long history ofaddressing a wide range of en-vironmental issues in the GreatLakes and other coastal envi-ronments. GLERL is the onlyNOAA research laboratory thathas the breadth of scientific ex-pertisetoaddresscomplexGreatLakes ecosystem issues. GLERLresearch and programs provideimportant information to deci-sion-makers and others to helpthem make good choices.

All of GLERL’s long-range re-search is targeted toward pro-ducing a suite of forecasts andforecastingcapabilitiesofphysi-calandecologicalconditionsthatwilladvanceanecosystem-basedapproach to management.

TheGreatLakesCoastalFore-castSystem,theGLCFSWebsite,(www.glerl.noaa.gov/res/glcfs/)

is a useful forecasting systemfor all users of the Great Lakescoastalwaterswhorequirereal-time information and forecastsoftemperatures,currents,waterlevels, and waves.

These forecasts provide Na-tional Weather Service marineforecasters with a significantsource of information, whichshould lead to considerable im-provementsbothintheaccuracyand efficiency of marine fore-casts for the Great Lakes.

GLERL also has exceptionalresources for teachers to makeGreat Lakes data more acces-sible and easy to use with theirstudents.GreatLakesWaterDataSets for Teachers (http://people.emich.edu/srutherf/NOAA/)con-tains real data extracted fromon-going and historic GLERLresearch projects, includingtemperature, dissolved oxygenand seiche data.

Data is in a format that is easyto use in the classroom. Middleor high school students andteachers can conduct their owninquiries, support guided inqui-ries, demonstrate limnologicalconcepts or just practice graph-ing, mapping and mathematicsusing real data.

A N N A M c C A R T N E Y ,Newspaper in Educationcoordinator, can be reached bye-mail.

Where to find marineforecasts, data, more

CONTRIBUTED GRAPHIC

Wind set-up is a local rise in water caused by winds pushing waterto one side of the lake. An extreme form of oscillation known as aseiche occurs when there are rapid changes in winds and barometricpressure. This diagram is from www.epa.gov/glnpo/atlas/glat-ch3.html.

By ANNA [email protected]

Tuesday, January 13, 2009 | Erie Times-News | GoErie.com | 3D