Managing Tidal Change: Project Report – Phase 1 FINAL May 2007
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OSTM/Jason-2 Products Handbook
OSTM/Jason-2 Products Handbook References: CNES : SALP-MU-M-OP-15815-CN EUMETSAT : EUM/OPS-JAS/MAN/08/0041 JPL: OSTM-29-1237 NOAA : Issue: 1 rev 0 Date: 17 June 2008 OSTM/Jason-2 Products Handbook Iss :1.0 - date : 17 June 2008 i.1 Chronology Issues: Issue: Date: Reason for change: 1rev0 June 17, 2008 Initial Issue People involved in this issue: Written by (*) : Date J.P. DUMONT CLS V. ROSMORDUC CLS N. PICOT CNES S. DESAI NASA/JPL H. BONEKAMP EUMETSAT J. FIGA EUMETSAT J. LILLIBRIDGE NOAA R. SHARROO ALTIMETRICS Index Sheet : Context: Keywords: Hyperlink: OSTM/Jason-2 Products Handbook Iss :1.0 - date : 17 June 2008 i.2 List of tables and figures List of tables: Table 1 : Differences between Auxiliary Data for O/I/GDR Products 1 Table 2 : Summary of error budget at the end of the verification phase 9 Table 3 : Main features of the OSTM/Jason-2 satellite 11 Table 4 : Mean classical orbit elements 16 Table 5 : Orbit auxiliary data 16 Table 6 : Equator Crossing Longitudes (in order of Pass Number) 18 Table 7 : Equator Crossing Longitudes (in order of Longitude) 19 Table 8 : Models and standards 21 Table 9 : CLS01 MSS model characteristics 22 Table 10 : CLS Rio 05 MDT model characteristics 23 Table 11 : Recommended editing criteria 26 Table 12 : Recommended filtering criteria 26 Table 13 : Recommended additional empirical tests 26 Table 14 : Main characteristics of (O)(I)GDR products 40 Table 15 - Dimensions used in the OSTM/Jason-2 data sets 42 Table 16 - netCDF variable type 42 Table 17 - Variable’s attributes 43 List of figures: Figure 1 -
Nitrogen Interception and Export by Experimental Salt Marsh Plots Exposed to Chronic Nutrient Addition
Vol. 400: 3–17, 2010 MARINE ECOLOGY PROGRESS SERIES Published February 11 doi: 10.3354/meps08460 Mar Ecol Prog Ser OPENPEN ACCESSCCESS FEATURE ARTICLE Nitrogen interception and export by experimental salt marsh plots exposed to chronic nutrient addition Lindsay D. Brin1, 2,*, Ivan Valiela2, Dale Goehringer3, Brian Howes3 1Brown University, Department of Ecology & Evolutionary Biology, 80 Waterman Street, Box G-W, Providence, Rhode Island 02912, USA 2The Ecosystems Center, Marine Biological Laboratory, 7 MBL St., Woods Hole, Massachusetts 02543, USA 3School of Marine Science and Technology, University of Massachusetts, Dartmouth, 706 South Rodney French Blvd., New Bedford, Massachusetts 02744, USA ABSTRACT: Mass balance studies conducted in the 1970s in Great Sippewissett Salt Marsh, New England, showed that fertilized plots intercepted 60 to 80% of the nitrogen (N) applied at several treatment levels every year from April to October, where interception mechanisms include plant uptake, denitrification and burial. These results pointed out that salt marshes are able to intercept land-derived N that could otherwise cause eutrophication in coastal waters. To determine the long-term N interception capacity of salt marshes and to assess the effect of different levels of N input, we measured nitrogenous materials in tidal water entering and leaving Great Sippewissett experimental plots in the 2007 growing season. Our results, from sampling over both full tidal cycles and more inten- sively sampled ebb tides, indicate high interception of Salt marshes limit the amount of land-derived nitrogen externally added N. Tidal export of dissolved inorganic carried by ebbing tides out to receiving coastal waters N (DIN) was small, although it increased with tide + Photo: Ivan Valiela height and at high N input rates. -
EXPLORER Official Visitors Guide
eFREE 2021 Official Visitors Guide Annapolis Rxploroyal & AreaerFREE Special Edition U BEYO D OQW TITEK A Dialongue of Place & D’iversity Page 2, explorer, 2021 Official Visitors Guide Come in and browse our wonderful assortment of Mens and Ladies apparel. Peruse our wide The unique Fort Anne Heritage Tapestry, designed by Kiyoko Sago, was stitched by over 100 volunteers. selection of local and best sellers books. Fort Anne Tapestry Annapolis Royal Kentville 2 hrs. from Halifax Fort Anne’s Heritage Tapestry How Do I Get To Annapolis Royal? Exit 22 depicts 4 centuries of history in Annapolis Holly and Henry Halifax three million delicate needlepoint Royal Bainton's stitches out of 95 colours of wool. It Tannery measures about 18’ in width and 8’ Outlet 213 St George Street, Annapolis Royal, NS Yarmouth in height and was a labor of love 19025322070 www.baintons.ca over 4 years in the making. It is a Digby work of immense proportions, but Halifax Annapolis Royal is a community Yarmouth with an epic story to relate. NOVA SCOTIA Planning a Visit During COVID-19 ANNAPOLIS ROYAL IS CONVENIENTLY LOCATED Folks are looking forward to Fundy Rose Ferry in Digby 35 Minutes travelling around Nova Scotia and Halifax International Airport 120 Minutes the Maritimes. “Historic, Scenic, Kejimkujik National Park & NHS 45 Minutes Fun” Annapolis Royal makes the Phone: 9025322043, Fax: 9025327443 perfect Staycation destination. Explorer Guide on Facebook is a www.annapolisroyal.com Convenience Plus helpful resource. Despite COVID19, the area is ready to welcome visitors Gasoline & Ice in a safe and friendly environment. -
BLAZING the TRAIL in NOVA SCOTIA in Canada’S Second Ook Up, Way Up, Because Glooscap Is a Giant in Atlantic Canada’S Mi’Kmaq Culture
article and photos by Jan Napier BLAZING THE TRAIL IN NOVA SCOTIA In Canada’s second ook up, way up, because Glooscap is a giant in Atlantic Canada’s Mi’kmaq culture. This almighty being was of such gargantuan proportions that the smallest province, a province of Nova Scotia was his bed and Prince Edward Island his pillow. larger-than-life demigod, Ancient legends of the mythical creator live on, and there’s no better place Lto explore them than the spectacular Glooscap Trail in northwestern Nova Scotia. over-the-top scenery and The trail stretches 227 miles, all told, but our itinerary focuses on a 125-mile the world’s highest tides segment between Truro and Joggins. It’s a laid-back, mostly coastal drive, beloved by those in the know. set the stage for RV The Mi’kmaq (pronounced Meeg-mah), an indigenous people native to travels on a grand scale Canada’s Maritime Provinces and the Gaspé Peninsula of Quebec, once lived freely in this region. Silas Tertius Rand, a Baptist missionary who traveled among the Mi’kmaq in the mid- to late-1800s, documented their stories featuring the heroic Glooscap. He “lived like other men ... but he never died, never was sick, never grew old,” wrote Rand. “He could do anything and everything.” Traveling RVers can learn more about Mi’kmaq myths and culture, and stand — dwarfed — beneath the demigod’s towering bronze likeness, at the Glooscap Heritage Centre, less than 5 miles from Truro in Millbrook. If you’re lucky, Climb Five Islands Lighthouse Program Director Gordon Pictou or a heritage interpreter will be on hand to for panoramic views of the Bay of Fundy, Minas Basin and the share some of the Mi’kmaq creation stories, like the one about Five Islands. -
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DFO — Libra ri ll joillue Restricted II I i 09070862 Environment Canada Environnement Canada RESOURCE DEVELOPMENT BRANCH MANUSCRIPT REPORT No. Atlantic Salmon Survey of Annapolis River System, Annapolis and Kings Counties,N.S. by J. Dalziel and N. MacEachern 4rittevice 11111111111111111111111111111111111111111111111111111111111111111111111111111111111111111111111111111111111 HolifoWN.S. ATLANTIC SALMON SURVEY OF ANNAPOLIS RIVER SYSTEM ANNAPOLIS & KINGS COS., N.S. 1957 by 3. Dalziel N. MacEachern ABSTRACT Good salmon spawning grounds were observed on the lower sections of the Nictaux River, Fales River and the South Annapolis River. A few scattered sections of possible spawning grounds exist on the main river between Lawrencetown and Paradise. Good nursery areas extend thr-aghout the snawning areas and includes all of the nain river. Major obstructions were found on all the large branch strepmR and include storage dams, barrier falls, mill dams and diversion canals. Salmon angling is carried out on the rain 7.iver - below -Aiddleton, on the Nictaux River, below Rogers Mill, and on the Lequille and Round Hill.7vers. GENERAL DESCRIPTION 07 STRUM The Annapolis Fiver is a comparatively large stream, about 50 miles long, which rises near Berwick, Kings County,'.3., and flows in a southerly direction through Kings and Annapolis Counties, emptying into Annapolis Basin below Annapolis Royal. The stream was surveyed during June and July, 1957, from Berwick West to the head of tide, including all of the main branch streams. Source to Middleton - From its source down to Mieldletonl the stream flows through neadowland and farmland with small sections of swampland and woodland scattered here and there. The gradient is slight, while the stream for the most part is gently flowing, broken occasionally by short, rapid sections. -
Puget Sound Dissolved Oxygen Modeling Study: Development of an Intermediate Scale Water Quality Model
Washington State Department of Ecology Publication No. 12-03-049 PNNL-20384 Rev 1 Prepared for the U.S. Department of Energy under Contract DE-AC05-76RL01830 Puget Sound Dissolved Oxygen Modeling Study: Development of an Intermediate Scale Water Quality Model by T Khangaonkar and W Long of the Pacific Northwest National Laboratory and B Sackmann, T Mohamedali, and M Roberts of the Washington State Department of Ecology November 2012 This page is purposely left blank This page is purposely left blank PNNL-20384 Rev 1 Puget Sound Dissolved Oxygen Modeling Study: Development of an Intermediate Scale Water Quality Model by T Khangaonkar and W Long of the Pacific Northwest National Laboratory B Sackmann, T Mohamedali, and M Roberts of the Washington State Department of Ecology October 2012 Prepared for the Washington State Department of Ecology under an Interagency Agreement with the U.S. Department of Energy Contract DE-AC05-76RL01830 Pacific Northwest National Laboratory Richland, Washington 99352 Any use of product or firm names in this publication is for descriptive purposes only and does not imply endorsement by the authors or the Department of Ecology. If you need this document in a format for the visually impaired, call 360-407-6764. Persons with hearing loss can call 711 for Washington Relay Service. Persons with a speech disability can call 877-833-6341. This page is purposely left blank Summary The Salish Sea, including Puget Sound, is a large estuarine system bounded by over seven thousand miles of complex shorelines, consists of several subbasins and many large inlets with distinct properties of their own. -
A Review of Ice and Tide Observations in the Bay of Fundy
A tlantic Geology 195 A review of ice and tide observations in the Bay of Fundy ConDesplanque1 and David J. Mossman2 127 Harding Avenue, Amherst, Nova Scotia B4H 2A8, Canada departm ent of Physics, Engineering and Geoscience, Mount Allison University, 67 York Street, Sackville, New Brunswick E4L 1E6, Canada Date Received April 27, 1998 Date Accepted December 15,1998 Vigorous quasi-equilibrium conditions characterize interactions between land and sea in macrotidal regions. Ephemeral on the scale of geologic time, estuaries around the Bay of Fundy progressively infill with sediments as eustatic sea level rises, forcing fringing salt marshes to form and reform at successively higher levels. Although closely linked to a regime of tides with large amplitude and strong tidal currents, salt marshes near the Bay of Fundy rarely experience overflow. Built up to a level about 1.2 m lower than the highest astronomical tide, only very large tides are able to cover the marshes with a significant depth of water. Peak tides arrive in sets at periods of 7 months, 4.53 years and 18.03 years. Consequently, for months on end, no tidal flooding of the marshes occurs. Most salt marshes are raised to the level of the average tide of the 18-year cycle. The number of tides that can exceed a certain elevation in any given year depends on whether the three main tide-generating factors peak at the same time. Marigrams constructed for the Shubenacadie and Cornwallis river estuaries, Nova Scotia, illustrate how the estuarine tidal wave is reshaped over its course, to form bores, and varies in its sediment-carrying and erosional capacity as a result of changing water-surface gradients. -
How a Tide Clock Works.Pub
Conventional time clocks have a 12 hour cycle, with 1 hand for hours, another for minutes. Tide clocks have a single hand, and a cycle of 12 hours 25 minutes, coinciding to an average time of about 6 hours 12 minutes between high and low tides. High tide is indicated when the hand is at the ‘12 o’clock’ position, low tide is indicated with the hand at the ‘6 o’clock’ position. A tide clock is not indicating 6 or 12 o’clock of course. It is merely a convenient reference point on the dial, showing us when our local tide is high or low. 12 is marked as High, 6 is marked as Low. However, the hour markings on the dial between the High and Low tide points do show us the number of hours since the last high or low tide, and the hours before the next high or low tide. A tide clock which has been initially set correctly will continue to display tide predictions quite accurately, requiring resetting only at intervals of about 4 months, depending upon the location. A brief explanation of how the tidal cycle works The Moon is the major cause of the tides. The ‘lunar day’ (the time it takes for the Moon to re-appear at the same place in the sky) is 24 hours and 50 minutes. New Zealand, and many other places in the world, have 2 high tides and 2 low tides each day. These are called semi-diurnal tides. Some areas of the world (eg Freemantle in Australia), have only one tide cycle per day, known as diurnal tides. -
Information to Users
INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy sutwnitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6" x 9" black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. ProQuest Information and Learning 300 North Zeeb Road. Ann Arbor, Ml 48106-1346 USA 800-521-0600 UMI ‘‘Sustainable Tourism for Smali Towns in the Maritimes’ A thesis submitted by Shaimna Mowatt-Densmore in partial fulfillment of the requirements for the degree of Master of Arts in Atlantic Canada Studies at Saint Mary’s University, Halifax, Nova Scotia. April 2001 Approved by: r. James H. Morrisdn -supervisor) Dr. -
Minas Basin, N.S
An examination of the population characteristics, movement patterns, and recreational fishing of striped bass (Morone saxatilis) in Minas Basin, N.S. during summer 2008 Report prepared for Minas Basin Pulp and Power Co. Ltd. Contributors: Jeremy E. Broome, Anna M. Redden, Michael J. Dadswell, Don Stewart and Karen Vaudry Acadia Center for Estuarine Research Acadia University Wolfville, NS B4P 2R6 June 2009 2 Executive Summary This striped bass study was initiated because of the known presence of both Shubenacadie River origin and migrant USA striped bass in the Minas Basin, the “threatened” species COSEWIC designation, the existence of a strong recreational fishery, and the potential for impacts on the population due to the operation of in- stream tidal energy technology in the area. Striped bass were sampled from Minas Basin through angling creel census during summer 2008. In total, 574 striped bass were sampled for length, weight, scales, and tissue. In addition, 529 were tagged with individually numbered spaghetti tags. Striped bass ranged in length from 20.7-90.6cm FL, with a mean fork length of 40.5cm. Data from FL(cm) and Wt(Kg) measurements determined a weight-length relationship: LOG(Wt) = 3.30LOG(FL)-5.58. Age frequency showed a range from 1-11 years. The mean age was 4.3 years, with 75% of bass sampled being within the Age 2-4 year class. Total mortality (Z) was estimated to be 0.60. Angling effort totalling 1732 rod hours was recorded from June to October, 2008, with an average 7 anglers fishing per tide. Catch per unit effort (Fish/Rod Hour) was determined to be 0.35, with peak landing periods indicating a relationship with the lunar cycle. -
Field Trips Guide Book for Photographers Revised 2008 a Publication of the Northern Virginia Alliance of Camera Clubs
Field Trips Guide Book for Photographers Revised 2008 A publication of the Northern Virginia Alliance of Camera Clubs Copyright 2008. All rights reserved. May not be reproduced or copied in any manner whatsoever. 1 Preface This field trips guide book has been written by Dave Carter and Ed Funk of the Northern Virginia Photographic Society, NVPS. Both are experienced and successful field trip organizers. Joseph Miller, NVPS, coordinated the printing and production of this guide book. In our view, field trips can provide an excellent opportunity for camera club members to find new subject matter to photograph, and perhaps even more important, to share with others the love of making pictures. Photography, after all, should be enjoyable. The pleasant experience of an outing together with other photographers in a picturesque setting can be stimulating as well as educational. It is difficullt to consistently arrange successful field trips, particularly if the club's membership is small. We hope this guide book will allow camera club members to become more active and involved in field trip activities. There are four camera clubs that make up the Northern Virginia Alliance of Camera Clubs McLean, Manassas-Warrenton, Northern Virginia and Vienna. All of these clubs are located within 45 minutes or less from each other. It is hoped that each club will be receptive to working together to plan and conduct field trip activities. There is an enormous amount of work to properly arrange and organize many field trips, and we encourage the field trips coordinator at each club to maintain close contact with the coordinators at the other clubs in the Alliance and to invite members of other clubs to join in the field trip. -
2019 Bay of Fundy Guide
VISITOR AND ACTIVITY GUIDE 2019–2020 BAYNova OF FUNDYScotia’s & ANNAPOLIS VALLEY TIDE TIMES pages 13–16 TWO STUNNING PROVINCES. ONE CONVENIENT CROSSING. Digby, NS – Saint John, NB Experience the phenomenal Bay of Fundy in comfort aboard mv Fundy Rose on a two-hour journey between Nova Scotia and New Brunswick. Ferries.ca Find Yourself on the Cliffs of Fundy TWO STUNNING PROVINCES. ONE CONVENIENT CROSSING. Digby, NS – Saint John, NB Isle Haute - Bay of Fundy Experience the phenomenal Bay of Fundy in comfort aboard mv Fundy Rose on a two-hour journey between Nova Scotia Take the scenic route and fi nd yourself surrounded by the and New Brunswick. natural beauty and rugged charm scattered along the Fundy Shore. Find yourself on the “Cliffs of Fundy” Cape D’or - Advocate Harbour Ferries.ca www.fundygeopark.ca www.facebook.com/fundygeopark Table of Contents Near Parrsboro General Information .................................. 7 Top 5 One-of-a-Kind Shopping ........... 33 Internet Access .................................... 7 Top 5 Heritage and Cultural Smoke-free Places ............................... 7 Attractions .................................34–35 Visitor Information Centres ................... 8 Tidally Awesome (Truro to Avondale) ....36–43 Important Numbers ............................. 8 Recommended Scenic Drive ............... 36 Map ............................................... 10–11 Top 5 Photo Opportunities ................. 37 Approximate Touring Distances Top Outdoor Activities ..................38–39 Along Scenic Route .........................10