How often does dissolved oxygen (DO) in the estuary fall below 5 mg/l?

Similar documents
How many adult oysters are in the Great Bay Estuary and how has it changed over time?

2017 Oyster Conservationist Report

Oyster Bed Mapping in the Great Bay Estuary,

Real Time Water Quality Report Main River at Paradise Pool

Government of Newfoundland and Labrador Department of Environment and Conservation Water Resources Management Division

Video-Based Mapping of Oyster Bottom in the Upper Piscataqua River, Sturgeon Creek, and Spruce Creek

COOPERATIVE LAKES MONITORING PROGRAM TRAINING FOR. Dissolved Oxygen and Temperature

FIU Digital Commons. Florida International University. Henry O. Briceño Florida International University,

(ml/l), (mg/l) or (ppm)

Executive Summary. Page Annual Program Report on NH Oyster Restoration 12/23/14

Overview. Learning Objectives

SALINITY. It's the amount of dissolved salts the water contains.

Potomac River Water Quality: Current Status & Trends

Executive Summary. New Hampshire ASMFC River Herring Sustainable Fishing Plan New Hampshire Fish and Game Department March, 2011.

2005 Shellfish Indicator Report

Warm-up # 7 A day 5/17 - B day 5/18 UPDATE YOUR TABLE OF CONTENTS

CHAPTER 11.1 THE WORLD OCEAN MARINE BIOMES NOTES

Water Quality Monitoring Using a Handheld Sonde for in situ Measurements Date Prepared: 11/17/2017

Rainbow Smelt. Appendix A: Fish. Osmerus mordax. New Hampshire Wildlife Action Plan Appendix A Fish-125

New Hampshire ASMFC River Herring Sustainable Fishing Plan New Hampshire Fish and Game Department March, Executive Summary

How does climate change make fish late for dinner?

NATIVE OYSTER RESTORATION AT ELKHORN SLOUGH, CALIFORNIA Summary of Elkhorn Slough National Estuarine Research Reserve and Elkhorn Slough Foundation

Shellfish Spotlight: 2008

ATLANTIC STATES MARINE FISHERIES COMMISSION. Winter Flounder Abundance and Biomass Indices from State Fishery-Independent Surveys

Hydraulic Modeling Analysis

Salinity and Dissolved Oxygen (D.O.) Lecture 2

Examples of estuaries include bays, sounds, salt marshes, mangrove forests, mud flats, swamps, inlets, and sloughs.

Refined Designated Uses for the Chesapeake Bay and Tidal Tributaries

Managing Development and Chesapeake Bay s Estuarine Fish

7.4 Temperature, Salinity and Currents in Jamaica Bay

Experiment C-6 Gas Solubility

Chemistry and Water Quality

FINAL REPORT APPENDIX A. Physical Description of the Shubenacadie River

2003 Horseshoe Beach Lease Area, Dixie County Quality Assurance/Quality Control (QA/QC) Log

Lecture 8 questions and answers The Biological Pump

Well, Well, Well. BACKGROUND Seasonal upwelling is a very important process in the coastal ocean of the Pacific Northwest.

Lesson 3: Which fish should I eat?

Marine Ecosystems. Aquatic Ecosystems Section 2

RESOLUTION MEPC.162(56) Adopted on 13 July 2007 GUIDELINES FOR RISK ASSESSMENT UNDER REGULATION A-4 OF THE BWM CONVENTION (G7)

N.H. Sea Grant Research Project Post Completion Report For time period 2/1/15 1/31/16

Water Quality Guidelines for Total Gas Pressure: First Update

Questions # 4 7 refer to Figure # 2 (page 321, Fig )

What does the % represent on the beakers?

Managing Chesapeake Bay s Land Use, Fish Habitat, and Fisheries: Studies. Jim Uphoff & Margaret McGinty, Fisheries Service

Notebooks or journals for drawing and taking notes

Significant Ecological Marine Area Assessment Sheet

EcoLogic Memorandum. TO: Ben Brezell; EDR FROM: Mark Arrigo RE: Possible Impacts of Dredging Snooks Pond DATE: 6/4/07

Time series topic 2: Decomposition

Beach. Coastal Fishing

Lamprey Rivers Advisory Committee (LRAC) Annual Report FY 2017 (Oct. 1, 2016 Sept. 30, 2017)

What happens to Oregon s tidal wetlands with sea level rise?

Zooplankton Migration Patterns at Scotton Landing: Behavioral Adaptations written by Lauren Zodl, University of Delaware

Annual Progress Report Overwintering Results of Ten Aerated Lakes in the Northwest Boreal Region

volvooceanrace.com Volvo Ocean Race Science programme Preliminary results Legs 10 and 11 Cardiff - Gothenburg - The Hague

Fine-Scale Survey of Right and Humpback Whale Prey Abundance and Distribution

Coral Reefs Lecture Notes

COUPLED MANAGEMENT STRATEGY LAKE CATHIE ESTUARY & COAST

Green crabs: invaders in the Great Marsh Featured scientist: Alyssa Novak from the Center for Coastal Studies/Boston University

NOTICE OF DECISION. DATE: April 16, 2018

EVALUATING THE EFFECTS OF BIVALVE SHELLFISH AQUACULTURE AND ITS ECOLOGICAL ROLE IN THE ESTUARINE ENVIRONMENT IN THE UNITED STATES

Chesapeake Bay Instantaneous Minimum Dissolved Oxygen Criteria: History and Background

RECREATIONAL PONDS AND LAKES

Project Webpage:

Instrumented Ballast Tank Studies to Examine Ballast Management Practices

Purpose: Hypothesis: Procedure:

State of New Hampshire's Estuaries

Blue crab ecology and exploitation in a changing climate.

Return. of the. Restored access leads to record runs up the Lamprey River. Michael Dionne

Grade 8 Science. Unit 1: Water Systems on Earth Chapter 3

170 points. 38 points In your textbook, read about modern oceanography. For each item write the word that meets the description.

East Central Florida Region Matt Culver, Brevard County James Gray, Indian River County Jim Oppenbourn, St. Lucie County Kathy Fitzpatrick, Martin

Causes and Monitoring of Hypoxia in Corpus Christi Bay

The Chesapeake Bay as an Estuary: An introduction. Istvan A. Urcuyo Gettysburg College

SEA GRANT PROGRESS REPORT

Worksheet: Solubility

Red Tide Blooms in Casco Bay (2010 State of the Bay Presentation)

Survival in an Estuary. Life in a Transition Zone

PRODUCT SHEET. Order probe only as RXPROBE02

SOME WATER CHARACTERISTICS OF ESTUARIES IN INDONESIA

Bay of Fundy Estuary Profile

Diadromous Fish Assemblage Assessment in the Saco River Estuary, ME

Types of Estuaries and Mixing Patterns. Mrs. Stahl Marine Science Honors

Ups and Downs in an Estuary

Types of Freshwater Ecosystems. Streams originate from underground water. Rivers form when streams join together. Freshwater Biome

National Marine Fisheries Service, Habitat Conservation Division:

Redondo Pier Alternate Site Activity

What s UP in the. Pacific Ocean? Learning Objectives

5/8/2018. Estuaries are classified by: > Mode of formation e.g. glaciers, deposition, sea level rise. > Patterns of water circulation

DOC/DON Reference Materials

Mark L. Botton and Robert E. Loveland. The Importance of Horseshoe Crabs in the Ecology of Delaware Bay: More than Just Bird Food?

NOAA Marine Fisheries and Research

Great Bay National Estuarine Research Reserve Field Notes Summer 2010 Welcome

Vertical in situ profiles of nitrate and oxygen in the northern Japan Sea

SOCIETAL GOALS TO DETERMINE ECOSYSTEM HEALTH: A FISHERIES CASE STUDY IN GALVESTON BAY SYSTEM, TEXAS

Instruction Sheet. Important Note: Information that requires special emphasis. Note: Information that supplements points in the main text.

Nortek Technical Note No.: TN-021. Chesapeake Bay AWAC Evaluation

Exploring Localized Mixing Dynamics During Wet Weather in a Tidal Fresh Water System

Dissolved Oxygen in Quahog Bay, ME

Monitoring Hypoxia Conditions in Corpus Christi Bay

Simulation of hydraulic regime and sediment transport in the Mekong delta coast

Transcription:

Indicator: Dissolved oxygen in the Great Bay Estuary Question How often does dissolved oxygen (DO) in the estuary fall below 5 mg/l? Short Answer Datasondes, an automated water quality sensor or probe, in the bays and open waters located at the center of the Great Bay and in Portsmouth Harbor at the Coastal Marine Laboratory indicate dissolved oxygen levels well above 5 mg/l. Low dissolved oxygen events occur in all the tidal rivers. In August 215 the most recent year we have data most low dissolved oxygen events in the tidal rivers lasted between two and six hours. PREP Goal Reduce nutrient loads to the estuaries and the ocean so that adverse, nutrient-related effects do not occur (from the PREP Comprehensive Conservation and Management Plan, PREP 2). Why This Matters Fish and many other organisms need dissolved oxygen in the water to survive. Dissolved oxygen levels can decrease due to various factors, including rapid changes in temperature and salinity, as well as respiration of organic matter. Dissolved oxygen levels can also decrease as a reaction to nutrient inputs. When nutrient loading is too high, phytoplankton and/or seaweed can bloom and then die. Bacteria and other decomposer organisms then use oxygen to break down the organic matter. Explanation (from 218 State of Our Estuaries Report) National ecosystem health thresholds for dissolved oxygen (DO) concentrations range from 2 mg/l to 5 mg/l, depending on the region or state (US EPA 212). The threshold of 5 mg/l is considered protective of all organisms (Bierman et al. 214). Dissolved oxygen levels in Great Bay at the central datasonde and in Portsmouth Harbor at the Coastal Marine Laboratory (Table DO-1; Figure DO-6) remain consistently above 5 mg/l. The most recently collected data from 215 show that DO concentrations never fell below 6 mg/l at these two sites. The tidal portions of the major tributary rivers continue to experience many days when the minimum DO concentration value is below 5 mg/l. No long-term trends are notable at any stations, as exemplified by the data from the Squamscott River and Salmon Falls River datasondes (Figures DO-1 and DO-2). These datasondes were used in this long-term trend analysis because they had complete datasets going back as far as 24, and because they represent different parts of the estuary. It is important to note not only the number of low DO events but also the duration of those events because there are implications for organisms (such as small invertebrates in the sediment) that cannot move quickly to areas with higher DO levels. In 215, the Lamprey and Squamscott Rivers had the highest number of low DO events, the majority of which took place in August and September. Figure DO-3 shows data taken every 15 minutes throughout August 215 for the Squamscott River; this figure indicates that DO concentrations fell below 5 mg/l most days during the month, and that there was less than 5 mg/l for 12% of the month. These low DO events lasted anywhere from one to four hours. In August 215, 73% of the time Lamprey River DO levels were below 5 mg/l and stayed below the threshold for more than 24 hours on two occasions (Figure DO-4) with the second occasion 93

35 at Squamscott River Datasonde (Number of days when minimum DO fell below 5 mg/l) 3 August Days 25 2 15 5 No Data Days Min >5 mg Days Min <5mg 24 29 212 214 215 Year Figure DO-1. Number of days in August when minimum DO fell below 5 mg/l at the Squamscott River datasonde. Particular years shown have the most complete datasets. 35 3 at Salmon Falls River Datasonde (Number of days when minimum DO fell below 5 mg/l) August Days 25 2 15 5 No Data Days Min >5 mg Days Min <5mg 24 29 212 214 215 Year Figure DO-2. Number of August days when minimum DO fell below 5 mg/l at the Salmon Falls River datasonde. Particular years shown have the most complete datasets. 94

lasting almost 168 hours (7 days). A 25 study (Pennock 25) of the Lamprey River concluded that the datasonde readings were reflective of river conditions, but that density stratification when salt water and fresh water stack in layers without mixing was a significant factor in the low DO conditions in the Lamprey River. Concentration (mg/l) 11 9 8 7 6 5 4 3 2 1 Squamscott River August 215 8/4 8/4 8/5 8/6 8/7 8/8 8/9 8/ 8/11 8/12 8/13 8/14 8/15 8/15 8/16 8/17 8/18 8/19 8/2 8/21 8/22 8/23 8/24 8/25 8/26 8/26 8/27 8/28 8/29 8/3 Figure DO-3. Dissolved oxygen concentration measurements at the Squamscott River datasonde, taken every 15 minutes during the month of August 215. The red line marks the 5 mg/l value; levels below this line may present a danger to fish and benthic invertebrates. The black arrow points to an event that represents approximately 1 hour below 5 mg/l. The gray arrow indicates an event that represents approximately 4 hours below 5 mg/l. In August 215, the Oyster River experienced four low DO events, lasting between two and six hours each. The Salmon Falls River experienced two low DO events, each lasting approximately three hours. In the Cocheco River, data was only available for the month of September 215. In that month, the datasonde indicates 12 low DO events, all lasting approximately two hours. More data and analysis is required to understand the relative importance of temperature, tidal stage, time of day, freshwater inputs, organic matter loading and nutrient loading as contributing factors to these low DO events. Finally, this analysis does not include all DO data collected in the Great Bay Estuary. For information on other data, please see the 217 Technical Support Document for Aquatic Life Use Support (NH DES 217). Methods and Data Sources In a system as well mixed as the Great Bay Estuary, low DO events may occur rapidly. Therefore, DO measurements taken at a high frequency by in-situ datasondes deployed 1-2 meters above the sediments were used for this indicator. 95

Concentration (mg/l) 11 9 8 7 6 5 4 3 2 1 Lamprey River August 215 8/1 8/2 8/3 8/4 8/5 8/6 8/7 8/8 8/9 8/ 8/11 8/12 8/13 8/14 8/15 8/16 8/17 8/18 8/19 8/2 8/21 8/22 8/23 8/24 8/26 8/27 8/28 8/29 8/3 8/31 Figure DO-4. Dissolved oxygen concentration measurements at the Lamprey River datasonde, taken every 15 minutes during the month of August. The red line marks the 5 mg/l value; levels below this line may present a danger to fish and benthic invertebrates. The black arrow points to one event (August 18) that represents approximately 3 hours below 5 mg/l. The gray arrow represents a longer event of below 5 mg/l conditions, lasting approximately 7 days. The daily minimum dissolved oxygen concentration were calculated at each station in the Great Bay Estuary (Figure DO-5). The number of days per year that the daily minimum DO fell below 5 mg/l was tabulated and is reported in Table DO-1. Inter-annual comparisons of that data are shown in Figure DO-6. The Great Bay National Estuarine Research Reserve Datasonde Program and the UNH Datasonde Program provided data for this indicator. The data used for this indicator were quality assured by staff from the UNH Jackson Estuarine Lab and NHDES. For data from 24 and later, the dissolved oxygen measurements were validated by pre- and post-deployment checks with an independently calibrated dissolved oxygen sensor or post-deployment calibration checks in the laboratory. For earlier years, for which quality control data were not available, only measurements from the first 96 hours of the sonde deployment were used. This is due to the fact that the older type of DO membrane-style probes had a tendency to drift over time. Technical Advisory Committee (TAC) Discussion Highlights For more information on the PREP TAC, please see: http://prepestuaries.org/prep-technical-advisory-committee/ With regard to the low DO events in the tributaries, the committee was divided in terms of how to interpret the dissolved oxygen data. Some TAC members see the occurrence of low DO events as indicators of high productivity and potential water quality problems related to excess nutrients and point to supersaturation events as an indication of this. Others feel more caution is required in the interpretation of the data, noting that low DO events can relate to stratification, 96

rainfall/runoff conditions, diurnal conditions, and changes in wind patterns. However, there is wider agreement that regardless of the cause of the low DO, these events are of concern to the resiliency of the system and may be of detriment to the organisms that live within it. With regard to comparing DO conditions between different stations, most of the TAC members urged caution, noting that the locations of the datasondes are not consistent in terms of distance from the mouths of the river (Figure DO-5). For example, the Oyster and Lamprey River stations are located fairly far up river, while the Squamscott River station is located at the mouth of the river. References Cited Bierman VJ, Diaz RJ, Kenworthy WJ, Reckhow KH. 214. Joint Report of Peer Review Panel for Numeric Nutrient Criteria for Great Bay Estuary. http://scholars.unh.edu/rtr/1/ NH DES. 217. Technical Support Document for the Great Bay Estuary Aquatic Life Use Support Assessments, 216 35(b) Report/33(d) List. https://www.des.nh.gov/organization/divisions/water/wmb/swqa/216/documents/r-wd-17-12.pdf Pennock J. 25. Lamprey River Study: A final report to the NH Estuaries Project. University of New Hampshire, Durham, NH. http://scholars.unh.edu/cgi/viewcontent.cgi?article=1185&context=prep PREP 2. Piscataqua Region Comprehensive Conservation and Management Plan, Piscataqua Region Estuaries Partnership: D.B.Truslow Associates, Mettee Planning Consultants, 2, Durham, NH. http://scholars.unh.edu/prep/22/ US EPA. 212. National Coastal Condition Report IV. https://www.epa.gov/national-aquaticresource-surveys/national-coastal-condition-report-iv-212 97

Table DO-1: Measurements of dissolved oxygen concentrations less than 5 mg/l at datasondes in the Great Bay Estuary. Station Year Number of Summer Days with Valid DO Data (Max of 92) Number of Summer Days with Minimum DO <5 mg/l Portsmouth Harbor 22 16 (of 16) Portsmouth Harbor 23 2 (of 2) Portsmouth Harbor 24 21 (of 21) Portsmouth Harbor 25 49 (of 49) Portsmouth Harbor 26 51 (of 51) Portsmouth Harbor 27 15 (of 15) Portsmouth Harbor 28 92 (of 92) Portsmouth Harbor 29 92 (of 92) Portsmouth Harbor 2 88 1 (of 88) Portsmouth Harbor 211 92 (of 92) Portsmouth Harbor 212 92 (of 92) Portsmouth Harbor 213 27 (of 27) Portsmouth Harbor 214 81 (of 81) Portsmouth Harbor 215 92 (of 92) Great Bay 2 9 (of 9) Great Bay 21 2 (of 2) Great Bay 22 29 (of 29) Great Bay 23 24 (of 24) Great Bay 24 2 (of 2) Great Bay 25 47 (of 47) Great Bay 26 59 (of 59) Great Bay 27 92 (of 92) Great Bay 28 92 (of 92) Great Bay 29 92 (of 92) Great Bay 2 8 (of 8) Great Bay 211 74 (of 74) Great Bay 212 85 9 (of 85) Great Bay 213 59 (of 59) Great Bay 214 69 (of 69) Great Bay 215 9 (of 9) Lamprey River 2 7 (of 7) Lamprey River 21 2 3 (of 2) Lamprey River 22 25 21 (of 25) Lamprey River 23 15 9 (of 15) Lamprey River 24 52 33 (of 52) Lamprey River 25 44 (of 44) Lamprey River 26 55 1 (of 55) Lamprey River 27 92 49 (of 92) Lamprey River 28 92 12 (of 92) Lamprey River 29 77 1 (of 77) Lamprey River 2 92 87 (of 92) Lamprey River 211 92 51 (of 92) Lamprey River 212 92 55 (of 92) Lamprey River 213 92 2 (of 92) 98

Station Year Number of Summer Days with Valid DO Data (Max of 92) Number of Summer Days with Minimum DO <5 mg/l Lamprey River 214 87 23 (of 87) Lamprey River 215 92 62 (of 92) Oyster River 22 25 9 (of 25) Oyster River 23 19 1 (of 19) Oyster River 24 52 21 (of 52) Oyster River 25 35 2 (of 35) Oyster River 26 3 1 (of 3) Oyster River 27 92 4 (of 92) Oyster River 28 53 7 (of 53) Oyster River 29 92 3 (of 92) Oyster River 2 12 2 (of 12) Oyster River 211 92 31 (of 92) Oyster River 212 86 9 (of 86) Oyster River 213 91 34 (of 91) Oyster River 214 91 (of 91) Oyster River 215 92 8 (of 92) Salmon Falls River 22 (of ) Salmon Falls River 23 17 6 (of 17) Salmon Falls River 24 6 12 (of 6) Salmon Falls River 25 1 (of ) Salmon Falls River 26 28 (of 28) Salmon Falls River 27 15 1 (of 15) Salmon Falls River 28 41 2 (of 41) Salmon Falls River 29 78 4 (of 78) Salmon Falls River 2 25 7 (of 25) Salmon Falls River 211 45 8 (of 45) Salmon Falls River 212 77 31 (of 77) Salmon Falls River 213 79 2 (of 79) Salmon Falls River 214 83 (of 83) Salmon Falls River 215 62 4 (of 62) Squamscott River 2 15 4 (of 15) Squamscott River 21 2 (of 2) Squamscott River 22 2 8 (of 2) Squamscott River 23 18 8 (of 18) Squamscott River 24 92 19 (of 92) Squamscott River 25 37 4 (of 37) Squamscott River 26 73 12 (of 73) Squamscott River 27 92 7 (of 92) Squamscott River 28 88 14 (of 88) Squamscott River 29 92 (of 92) Squamscott River 2 8 36 (of 8) Squamscott River 211 92 25 (of 92) Squamscott River 212 92 25 (of 92) Squamscott River 213 92 28 (of 92) Squamscott River 214 83 27 (of 83) Squamscott River 215 87 51 (of 87) Note: Summer days are defined as days in the months of July, August, and September. Maximum is 92. 99

Figure DO-5: Map of datasonde station locations.

Figure DO-6: DO concentrations. Number of days in July, August, and September relative to 5 mg/l threshold. Monitoring Location (GRBGB) (black circle with white plus sign) at Great Bay Datasonde 9 8 7 6 5 4 3 2 2 21 22 23 24 25 26 27 28 29 2 211 212 213 214 215 Summer Days (Jul-Sep) Min Less Than 5 mg/l Min 5 mg/l or Higher No Data Station: GRBGB (Great Bay). Maximum number of days is 92. 1

at Lamprey River Datasonde Monitoring Location (GRBLR) (black circle with white plus sign) 9 8 7 6 5 4 3 2 2 21 22 23 24 25 26 27 28 29 2 211 212 213 214 215 Summer Days (Jul-Sep) Min Less Than 5 mg/l Min 5 mg/l or Higher No Data Station: GRBLR (Lamprey River). Maximum number of days is 92. 2

at Oyster River Datasonde Monitoring Location (GRBOR) (black circle with white plus sign) 9 8 7 6 5 4 3 2 22 23 24 25 26 27 28 29 2 211 212 213 214 215 Summer Days (Jul-Sep) Min Less Than 5 mg/l Min 5 mg/l or Higher No Data Station: GRBOR (Oyster River). Maximum number of days is 92. 3

at Salmon Falls River Datasonde Monitoring Location (GRBSF) (black circle with white plus sign) 9 8 7 6 5 4 3 2 22 23 24 25 26 27 28 29 2 211 212 213 214 215 Summer Days (Jul-Sep) Min Less Than 5 mg/l Min 5 mg/l or Higher No Data Station: GRBSF (Salmon Falls River). Maximum number of days is 92. 4

at Squamscott River Datasonde Monitoring Location (GRBSQ) (black circle with white plus sign) 9 8 7 6 5 4 3 2 2 21 22 23 24 25 26 27 28 29 2 211 212 213 214 215 Summer Days (Jul-Sep) Min Less Than 5 mg/l Min 5 mg/l or Higher No Data Station: GRBSQ (Squamscott River at the railroad trestle). Maximum number of days is 92. 5

at the Coastal Marine Laboratory (Portsmouth Harbor) Datasonde Monitoring Location (GRBCML) (black circle with white plus sign) 9 8 Summer Days (Jul-Sep) 7 6 5 4 3 2 22 23 24 25 26 27 28 29 2 211 212 213 214 215 Min Less Than 5 mg/l Year Min 5 mg/l or Higher No Data Station: GRBCML (Portsmouth Harbor at the Coastal Marine Laboratory). Maximum number of days is 92. 6