Dredging History of Southwest Florida Inland Waterways
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2019 Preliminary Manatee Mortality Table with 5-Year Summary From: 01/01/2019 To: 11/22/2019
FLORIDA FISH AND WILDLIFE CONSERVATION COMMISSION MARINE MAMMAL PATHOBIOLOGY LABORATORY 2019 Preliminary Manatee Mortality Table with 5-Year Summary From: 01/01/2019 To: 11/22/2019 County Date Field ID Sex Size Waterway City Probable Cause (cm) Nassau 01/01/2019 MNE19001 M 275 Nassau River Yulee Natural: Cold Stress Hillsborough 01/01/2019 MNW19001 M 221 Hillsborough Bay Apollo Beach Natural: Cold Stress Monroe 01/01/2019 MSW19001 M 275 Florida Bay Flamingo Undetermined: Other Lee 01/01/2019 MSW19002 M 170 Caloosahatchee River North Fort Myers Verified: Not Recovered Manatee 01/02/2019 MNW19002 M 213 Braden River Bradenton Natural: Cold Stress Putnam 01/03/2019 MNE19002 M 175 Lake Ocklawaha Palatka Undetermined: Too Decomposed Broward 01/03/2019 MSE19001 M 246 North Fork New River Fort Lauderdale Natural: Cold Stress Volusia 01/04/2019 MEC19002 U 275 Mosquito Lagoon Oak Hill Undetermined: Too Decomposed St. Lucie 01/04/2019 MSE19002 F 226 Indian River Fort Pierce Natural: Cold Stress Lee 01/04/2019 MSW19003 F 264 Whiskey Creek Fort Myers Human Related: Watercraft Collision Lee 01/04/2019 MSW19004 F 285 Mullock Creek Fort Myers Undetermined: Too Decomposed Citrus 01/07/2019 MNW19003 M 275 Gulf of Mexico Crystal River Verified: Not Recovered Collier 01/07/2019 MSW19005 M 270 Factory Bay Marco Island Natural: Other Lee 01/07/2019 MSW19006 U 245 Pine Island Sound Bokeelia Verified: Not Recovered Lee 01/08/2019 MSW19007 M 254 Matlacha Pass Matlacha Human Related: Watercraft Collision Citrus 01/09/2019 MNW19004 F 245 Homosassa River Homosassa -
Map of the Approximate Inland Extent of Saltwater at the Base of the Biscayne Aquifer in Miami-Dade County, Florida, 2018: U.S
U.S. Department of the Interior Scientific Investigations Map 3438 Prepared in cooperation with U.S. Geological Survey Sheet 1 of 1 Miami-Dade County Pamphlet accompanies map 80°40’ 80°35’ 80°30’ 80°25’ 80°20’ 80°15’ 80°10’ 80°05’ 0 5 10 KILOMETERS 1 G-3949S / 26 G-3949I / 144 0 5 10 MILES BROWARD COUNTY G-3949D / 225 MIAMI-DADE COUNTY EXPLANATION 2 G-3705 / 5,570 Well fields DMW6 / 42.7 IMW6 / 35 Approximate boundary of the Model Land Area DMW7 / 32 Approximate inland extent of saltwater in 2018—Isochlor represents a chloride IMW7 / 16.3 G-3948S / 151 concentration of 1,000 milligrams per liter at the base of the aquifer 3 G-3948D / 4,690 25°55’ G-3978 / 69 Dashed where data are insufficient Approximation 4 G-3601S / 330 G-3601I / 464 Approximate inland extent of saltwater in 2011 (Prinos and others, 2014)—Isochlor G-3601D (formerly G-3601) / 1,630 represents a chloride concentration of 1,000 milligrams per liter at the base of G-894 / 16 the aquifer Winson 1 / 31 F-279 / 4,700 Approximation Gratigny Well / 2,690 Dashed where data are insufficient Miami Canal G-297 (121 & 4th) / 19 5 3 ! Proposed locations for new wells and number (see table 4) G-3224 / 36 G-3705 / 5,570 ! Monitoring well name and chloride concentration, in milligrams per liter FLORIDA G-3602 / 5,250 G-3947 / 23 25°50’ F-45 / 175 Lake Okeechobee G-3250 / 187 6 G-548 / 32 G-3603 / 182 G-1354 / 920 Study area 7 G-571 / 27 G-3964 / 1,970 Florida Bay G-354 / 36 G-3704 / 8,730 G-1351 / 379 Miami International Airport 9 G-3604 / 6,860 G-3605 / 4,220 8 G-3977S / 17 G-3977D -
The Caloosahatchee River Estuary: a Monitoring Partnership Between Federal, State, and Local Governments, 2007–13
Prepared in cooperation with the Florida Department of Environmental Protection and the South Florida Water Management District The Caloosahatchee River Estuary: A Monitoring Partnership Between Federal, State, and Local Governments, 2007–13 By Eduardo Patino The tidal Caloosahatchee River and downstream estuaries also known as S–79 (fig. 2), which are operated by the USGS (fig. 1) have substantial environmental, recreational, and economic in cooperation with the U.S. Army Corps of Engineers, Lee value for southwest Florida residents and visitors. Modifications to County, and the City of Cape Coral. Additionally, a monitor- the Caloosahatchee River watershed have altered the predevelop- ing station was operated on Sanibel Island from 2010 to 2013 ment hydrology, thereby threatening the environmental health of (fig. 1) as part of the USGS Greater Everglades Priority Eco- estuaries in the area (South Florida Water Management District, system Science initiative and in partnership with U.S. Fish and 2014). Hydrologic monitoring of the freshwater contributions from Wildlife Service (J.N. Ding Darling National Wildlife Ref- tributaries to the tidal Caloosahatchee River and its estuaries is uge). Moving boat water-quality surveys throughout the tidal necessary to adequately describe the total freshwater inflow and Caloosahatchee River and downstream estuaries began in 2011 constituent loads to the delicate estuarine system. and are ongoing. Information generated by these monitoring From 2007 to 2013, the U.S. Geological Survey (USGS), in networks has proved valuable to the FDEP for developing total cooperation with the Florida Department of Environmental Protec- maximum daily load criteria, and to the SFWMD for calibrat- tion (FDEP) and the South Florida Water Management District ing and verifying a hydrodynamic model. -
Blue-Green Algal Bloom Weekly Update Reporting March 26 - April 1, 2021
BLUE-GREEN ALGAL BLOOM WEEKLY UPDATE REPORTING MARCH 26 - APRIL 1, 2021 SUMMARY There were 12 reported site visits in the past seven days (3/26 – 4/1), with 12 samples collected. Algal bloom conditions were observed by the samplers at seven of the sites. The satellite imagery for Lake Okeechobee and the Caloosahatchee and St. Lucie estuaries from 3/30 showed low bloom potential on visible portions of Lake Okeechobee or either estuary. The best available satellite imagery for the St. Johns River from 3/26 showed no bloom potential on Lake George or visible portions of the St. Johns River; however, satellite imagery from 3/26 was heavily obscured by cloud cover. Please keep in mind that bloom potential is subject to change due to rapidly changing environmental conditions or satellite inconsistencies (i.e., wind, rain, temperature or stage). On 3/29, South Florida Water Management District staff collected a sample from the C43 Canal – S77 (Upstream). The sample was dominated by Microcystis aeruginosa and had a trace level [0.42 parts per billion (ppb)] of microcystins detected. On 3/29, Florida Department of Environmental Protection (DEP) staff collected a sample from Lake Okeechobee – S308 (Lakeside) and at the C44 Canal – S80. The Lake Okeechobee – S308 (Lakeside) sample was dominated by Microcystis aeruginosa and had a trace level (0.79 ppb) of microcystins detected. The C44 Canal – S80 sample had no dominant algal taxon and had a trace level (0.34 ppb) of microcystins detected. On 3/29, Highlands County staff collected a sample from Huckleberry Lake – Canal Entrance. -
Late Holocene Sea Level Rise in Southwest Florida: Implications for Estuarine Management and Coastal Evolution
LATE HOLOCENE SEA LEVEL RISE IN SOUTHWEST FLORIDA: IMPLICATIONS FOR ESTUARINE MANAGEMENT AND COASTAL EVOLUTION Dana Derickson, Figure 2 FACULTY Lily Lowery, University of the South Mike Savarese, Florida Gulf Coast University Stephanie Obley, Flroida Gulf Coast University Leonre Tedesco, Indiana University and Purdue Monica Roth, SUNYOneonta University at Indianapolis Ramon Lopez, Vassar College Carol Mankiewcz, Beloit College Lora Shrake, TA, Indiana University and Purdue University at Indianapolis VISITING and PARTNER SCIENTISTS Gary Lytton, Michael Shirley, Judy Haner, STUDENTS Leslie Breland, Dave Liccardi, Chuck Margo Burton, Whitman College McKenna, Steve Theberge, Pat O’Donnell, Heather Stoffel, Melissa Hennig, and Renee Dana Derickson, Trinity University Wilson, Rookery Bay NERR Leda Jackson, Indiana University and Purdue Joe Kakareka, Aswani Volety, and Win University at Indianapolis Everham, Florida Gulf Coast University Chris Kitchen, Whitman College Beth A. Palmer, Consortium Coordinator Nicholas Levsen, Beloit College Emily Lindland, Florida Gulf Coast University LATE HOLOCENE SEA LEVEL RISE IN SOUTHWEST FLORIDA: IMPLICATIONS FOR ESTUARINE MANAGEMENT AND COASTAL EVOLUTION MICHAEL SAVARESE, Florida Gulf Coast University LENORE P. TEDESCO, Indiana/Purdue University at Indianapolis CAROL MANKIEWICZ, Beloit College LORA SHRAKE, TA, Indiana/Purdue University at Indianapolis PROJECT OVERVIEW complicating environmental management are the needs of many federally and state-listed Southwest Florida encompasses one of the endangered species, including the Florida fastest growing regions in the United States. panther and West Indian manatee. Watershed The two southwestern coastal counties, Collier management must also consider these issues and Lee Counties, commonly make it among of environmental health and conservation. the 5 fastest growing population centers on nation- and statewide censuses. -
Collier Miami-Dade Palm Beach Hendry Broward Glades St
Florida Fish and Wildlife Conservation Commission F L O R ID A 'S T U R N P IK E er iv R ee m Lakewood Park m !( si is O K L D INDRIO ROAD INDRIO RD D H I N COUNTY BCHS Y X I L A I E O W L H H O W G Y R I D H UCIE BLVD ST L / S FT PRCE ILT SRA N [h G Fort Pierce Inlet E 4 F N [h I 8 F AVE "Q" [h [h A K A V R PELICAN YACHT CLUB D E . FORT PIERCE CITY MARINA [h NGE AVE . OKEECHOBEE RA D O KISSIMMEE RIVER PUA NE 224 ST / CR 68 D R !( A D Fort Pierce E RD. OS O H PIC R V R T I L A N N A M T E W S H N T A E 3 O 9 K C A R-6 A 8 O / 1 N K 0 N C 6 W C W R 6 - HICKORY HAMMOCK WMA - K O R S 1 R L S 6 R N A E 0 E Lake T B P U Y H D A K D R is R /NW 160TH E si 68 ST. O m R H C A me MIDWAY RD. e D Ri Jernigans Pond Palm Lake FMA ver HUTCHINSON ISL . O VE S A t C . T I IA EASY S N E N L I u D A N.E. 120 ST G c I N R i A I e D South N U R V R S R iv I 9 I V 8 FLOR e V ESTA DR r E ST. -
South Florida Circumnavigation 2017
Completing the Circumnavigation of South Florida By Chuck Purse South Florida is actually an island! The nine day voyage began early in January, 2017 when we completed the first leg from Hillsboro Inlet to Stuart, FL about 85 miles north of the Club. We waited for a good day so that we could make the run in open water rather than the using the time consuming Intracoastal Waterway. We stayed at Sunset Bay Marina in Stuart, one of the prettiest places on the East Coast. The sunsets are indeed beautiful and all the needed services are available at a reasonable cost. Stuart offers a broad array of dining choices and the adorable Old Colorado Inn. The next day took us up the St Lucie River toward Lake Okeechobee. The Okeechobee Waterway runs 155 miles from Stuart westward through Lake Okeechobee to Ft Myers and the Gulf of Mexico. This Waterway separates the southern portion of the State from the northern part of the Florida peninsula. The crossing includes beautiful countryside, incredible wildlife, and five locks to navigate as you make the 15’ climb up to Lake Okeechobee. The lake itself is impressively large with only the southern shore visible as you cross. Be careful to stay in the channel especially when the lake level is low to minimize the chance of bouncing off the bottom! That night we stayed at Roland Martin Marina in Clewiston, FL bordering the southwestern corner of the the lake. This historical sugar town is worth a one night visit. We arrived in time to play golf at Clewiston Golf Course which was a pleasant surprise. -
Chapter 8C: St. Lucie and Caloosahatchee River Watersheds Annual Report
2019 South Florida Environmental Report – Volume I Chapter 8C Chapter 8C: St. Lucie and Caloosahatchee River Watersheds Annual Report Cassondra Armstrong, Fawen Zheng, Anna Wachnicka, Amanda Khan, Zhiqiang Chen, and Lucia Baldwin SUMMARY A description of the estuaries and the river watersheds is followed by a summary of the conditions of the hydrology (rainfall and flow), water quality (salinity, phosphorus, nitrogen, and chlorophyll a [Chla]), and aquatic habitat (oysters and submerged aquatic vegetation [SAV]) based on results of the Research and Water Quality Monitoring Programs (RWQMPs). Following the summary for each estuary, significant findings during the Water Year 2018 (WY2018; May 1, 2017–April 30, 2018) reporting period are highlighted. In addition, the St. Lucie and Caloosahatchee river watersheds’ water quality monitoring results for total phosphorus (TP) and total nitrogen (TN) by basin are presented in Appendix 8C-1 of this volume as supplemental information. ST. LUCIE ESTUARY WY2018 total annual rainfall across the Tier 1 Contributing Areas (Lake Okeechobee, St. Lucie Basin, and Tidal Basin) to the St. Lucie Estuary (SLE) was more than the long-term average from WY1997 through WY2018. Although 74% of the annual rainfall usually occurs in the wet season, this value increased to 80% in WY2018. The relatively high amount of wet season rain was the driver for increased discharge to the SLE. The total annual freshwater inflow to the SLE in WY2018 (1.6 million acre-feet [ac-ft]) was higher than the long-term average of 1.0 million ac-ft. The inflow and percent contribution from Lake Okeechobee in WY2018 (0.6 million ac-ft and 37%, respectively) were greater than the long-term averages (0.3 million ac-ft and 26%, respectively). -
An Historical Perspective on the Kissimmee River Restoration Project
ing of 14 km of river channel, and removal of two water An Historical control structures and associated levees. Restoration of the Kissimmee River ecosystem will result in the reestablish ment of 104 km2 of river-floodplain ecosystem, including Perspective on the 70 km of river channel and 11,000 ha of wetland habitat, which is expected to benefit over 320 species of fish and Kissimmee River wildlife. Restoration Project Background he Kissimmee River basin is located in central Florida Tbetween the city of Orlando and lake Okeechobee Joseph W. Koebel, Jr.1 within the Coastal Lowlands physiographic province. It con sists of a 4229-km2 upper basin, which includes Lake Kis Abstract simmee and 18 smaller lakes ranging in size from a few hec tares to 144 km2, and a 1,963-km2 lower basin, which This paper reviews the events leading to the channeliza includes the tributary watersheds (excluding Lake Istok tion of the Kissimmee River, the physical, hydrologic, and poga) of the Kissimmee River between lake Kissimmee and biological effects of channelization, and the restoration lake Okeechobee. The physiography of the region includes movement. Between 1962 and 1971, in order to provide the Osceola and Okeechobee Plains and the Lake Wales flood control for central and southern florida, the 166 ridge of the Wicomico shore (U.S. Army Corps of Engineers km-Iong meandering Kissimmee River was transformed 1992). into a 90 km-Iong, 10 meter-deep, 100 meter-wide canal. Prior to channelization, the Kissimmee River meandered Channelization and transformation of the Kissimmee River approximately 166 km within a 1.5-3-km-wide floodplain. -
Washington State National Maritime Heritage Area Feasibility Study for Designation As a National Heritage Area
Washington State National Maritime Heritage Area Feasibility Study for Designation as a National Heritage Area WASHINGTON DEPARTMENT OF ARCHAEOLOGY AND HISTORIC PRESERVATION Washington State National Maritime Heritage Area Feasibility Study for Designation as a National Heritage Area WASHINGTON DEPARTMENT OF ARCHAEOLOGY AND HISTORIC PRESERVATION APRIL 2010 The National Maritime Heritage Area feasibility study was guided by the work of a steering committee assembled by the Washington State Department of Archaeology and Historic Preservation. Steering committee members included: • Dick Thompson (Chair), Principal, Thompson Consulting • Allyson Brooks, Ph.D., Department of Archaeology and Historic Preservation • Chris Endresen, Office of Maria Cantwell • Leonard Forsman, Chair, Suquamish Tribe • Chuck Fowler, President, Pacific Northwest Maritime Heritage Council • Senator Karen Fraser, Thurston County • Patricia Lantz, Member, Washington State Heritage Center Trust Board of Trustees • Flo Lentz, King County 4Culture • Jennifer Meisner, Washington Trust for Historic Preservation • Lita Dawn Stanton, Gig Harbor Historic Preservation Coordinator Prepared for the Washington State Department of Archaeology and Historic Preservation by Parametrix Berk & Associates March , 2010 Washington State NATIONAL MARITIME HERITAGE AREA Feasibility Study Preface National Heritage Areas are special places recognized by Congress as having nationally important heritage resources. The request to designate an area as a National Heritage Area is locally initiated, -
C-43 Caloosahatchee River Watershed Protection Plan
Caloosahatchee River Watershed Protection Plan APPENDICES January 2009 APPENDICES A – Performance Measure and Performance Indicator Fact Sheets B – Management Measure Tool Box and Fact Sheets C – Northern Everglades Regional Simulation Model D – Nutrient Loading Rates, Reduction Factors and Implementation Costs Associated with BMPs and Technologies E – Caloosahatchee River Watershed Research and Water Quality Monitoring Program F – Plan Operations & Maintenance, Permitting, and Monitoring G – Potential Funding Sources H – Agency and Public Comments and Responses APPENDIX A PERFORMANCE MEASURE AND PERFORMANCE INDICATOR FACT SHEETS Appendix A Caloosahatchee River and Estuary Performance Measures Number of Times Caloosahatchee Estuary High Discharge Criteria Exceeded Performance Measure: Number of Times Caloosahatchee Estuary High Discharge Criteria Exceeded – Mean Monthly Flows >2,800 cfs and Mean Monthly Flows > 4,500 cfs Description – The Lake Okeechobee WSE Regulation Schedule is applied to regulate (flood control) discharges to the Caloosahatchee River, and subsequently to the Caloosahatchee Estuary, when lake stages are high. The Caloosahatchee River has primary capacity for local inflows and is only utilized for Caloosahatchee Estuary discharges when there is secondary capacity available. The number of times that the Caloosahatchee Estuary high discharge criterion is exceeded must be limited to prevent destructive impacts on the estuary. Rationale – Researchers have observed an increased rate of eutrophication in Lake Okeechobee from 1973 to the present. Symptoms of this eutrophication include the following: • increases in algal bloom frequency since the mid-1980s (with an algal bloom being defined as chlorophyll-a concentrations greater than 40 μg/L) (Maceina 1993, Carrick et al. 1994, Havens et al. 1995b), • increases in the dominance of blue-green algae following a shift in the TN:TP ratio (Smith et al. -
Environmental Plan for Kissimmee Okeechobee Everglades Tributaries (EPKOET)
Environmental Plan for Kissimmee Okeechobee Everglades Tributaries (EPKOET) Stephanie Bazan, Larissa Gaul, Vanessa Huber, Nicole Paladino, Emily Tulsky April 29, 2020 TABLE OF CONTENTS 1. BACKGROUND AND HISTORY…………………...………………………………………..4 2. MISSION STATEMENT…………………………………....…………………………………7 3. GOVERNANCE……………………………………………………………………...………...8 4. FEDERAL, STATE, AND LOCAL POLICIES…………………………………………..…..10 5. PROBLEMS AND GOALS…..……………………………………………………………....12 6. SCHEDULE…………………………………....……………………………………………...17 7. CONCLUSIONS AND RECOMMENDATIONS…………………………………………....17 REFERENCES…………………………………………………………..……………………....18 2 LIST OF FIGURES Figure A. Map of the Kissimmee Okeechobee Everglades Watershed…………………………...4 Figure B. Phosphorus levels surrounding the Kissimmee Okeechobee Everglades Watershed…..5 Figure C. Before and after backfilling of the Kissimmee river C-38 canal……………………….6 Figure D. Algae bloom along the St. Lucie River………………………………………………...7 Figure E. Florida’s Five Water Management Districts………………………………………........8 Figure F. Three main aquifer systems in southern Florida……………………………………....14 Figure G. Effect of levees on the watershed………………………………………...…………...15 Figure H. Algal bloom in the KOE watershed…………………………………………...………15 Figure I: Canal systems south of Lake Okeechobee……………………………………………..16 LIST OF TABLES Table 1. Primary Problems in the Kissimmee Okeechobee Everglades watershed……………...13 Table 2: Schedule for EPKOET……………………………………………………………….…18 3 1. BACKGROUND AND HISTORY The Kissimmee Okeechobee Everglades watershed is an area of about