Baseline Data on the Oceanography of Cook Inlet, Alaska
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North Pacific Research Board Project Final Report
NORTH PACIFIC RESEARCH BOARD PROJECT FINAL REPORT Synthesis of Marine Biology and Oceanography of Southeast Alaska NPRB Project 406 Final Report Ginny L. Eckert1, Tom Weingartner2, Lisa Eisner3, Jan Straley4, Gordon Kruse5, and John Piatt6 1 Biology Program, University of Alaska Southeast, and School of Fisheries and Ocean Sciences, University of Alaska Fairbanks, 11120 Glacier Hwy., Juneau, AK 99801, (907) 796-6450, [email protected] 2 Institute of Marine Science, University of Alaska Fairbanks, P.O. Box 757220, Fairbanks, AK 99775-7220, (907) 474-7993, [email protected] 3 Auke Bay Lab, National Oceanic and Atmospheric Administration, 17109 Pt. Lena Loop Rd., Juneau, AK 99801, (907) 789-6602, [email protected] 4 University of Alaska Southeast, 1332 Seward Ave., Sitka, AK 99835, (907) 774-7779, [email protected] 5 School of Fisheries and Ocean Sciences, University of Alaska Fairbanks, 11120 Glacier Hwy., Juneau, AK 99801, (907) 796-2052, [email protected] 6 Alaska Science Center, US Geological Survey, Anchorage, AK, 360-774-0516, [email protected] August 2007 ABSTRACT This project directly responds to NPRB specific project needs, “Bring Southeast Alaska scientific background up to the status of other Alaskan waters by completing a synthesis of biological and oceanographic information”. This project successfully convened a workshop on March 30-31, 2005 at the University of Alaska Southeast to bring together representatives from different marine science disciplines and organizations to synthesize information on the marine biology and oceanography of Southeast Alaska. Thirty-eight individuals participated, including representatives of the University of Alaska and state and national agencies. -
Tidal Hydrodynamic Response to Sea Level Rise and Coastal Geomorphology in the Northern Gulf of Mexico
University of Central Florida STARS Electronic Theses and Dissertations, 2004-2019 2015 Tidal hydrodynamic response to sea level rise and coastal geomorphology in the Northern Gulf of Mexico Davina Passeri University of Central Florida Part of the Civil Engineering Commons Find similar works at: https://stars.library.ucf.edu/etd University of Central Florida Libraries http://library.ucf.edu This Doctoral Dissertation (Open Access) is brought to you for free and open access by STARS. It has been accepted for inclusion in Electronic Theses and Dissertations, 2004-2019 by an authorized administrator of STARS. For more information, please contact [email protected]. STARS Citation Passeri, Davina, "Tidal hydrodynamic response to sea level rise and coastal geomorphology in the Northern Gulf of Mexico" (2015). Electronic Theses and Dissertations, 2004-2019. 1429. https://stars.library.ucf.edu/etd/1429 TIDAL HYDRODYNAMIC RESPONSE TO SEA LEVEL RISE AND COASTAL GEOMORPHOLOGY IN THE NORTHERN GULF OF MEXICO by DAVINA LISA PASSERI B.S. University of Notre Dame, 2010 A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Civil, Environmental, and Construction Engineering in the College of Engineering and Computer Science at the University of Central Florida Orlando, Florida Spring Term 2015 Major Professor: Scott C. Hagen © 2015 Davina Lisa Passeri ii ABSTRACT Sea level rise (SLR) has the potential to affect coastal environments in a multitude of ways, including submergence, increased flooding, and increased shoreline erosion. Low-lying coastal environments such as the Northern Gulf of Mexico (NGOM) are particularly vulnerable to the effects of SLR, which may have serious consequences for coastal communities as well as ecologically and economically significant estuaries. -
Tide Simplified by Phil Clegg Sea Kayaking Anglesey
Tide Simplified By Phil Clegg Sea Kayaking Anglesey Tide is one of those areas that the more you learn about it, the more you realise you don’t know. As sea kayakers, and not necessarily scientists, we don’t have to know every detail but a simplified understanding can help us to understand and predict what we might expect to see when we are out on the water. In this article we look at the areas of tide you need to know about without having to look it up in a book. Causes of tides To understand tide is convenient to imagine the earth with an envelope of water all around it, spinning once every 24 hours on its north-south axis with the moon on a line parallel to the equator. Moon Gravity A B Earth Ocean C The tides are primarily caused by the gravitational attraction of the moon. Simplifying a bit, at point A the gravitational pull is the strongest causing a high tide, point B experiences a medium pull towards the moon, while point C has the weakest pull causing a second high tide. Because the earth spins once every 24 hours, at any location on its surface there are two high tides and two low tides a day. There are approximately six hours between high tide and low tide. One way of predicting the approximate time of high tide is to add 50 minutes to the high tide of the previous day. The sun has a similar but weaker gravitational effect on the tides. On average this is about 40 percent of that of the moon. -
Chapter 5 Water Levels and Flow
253 CHAPTER 5 WATER LEVELS AND FLOW 1. INTRODUCTION The purpose of this chapter is to provide the hydrographer and technical reader the fundamental information required to understand and apply water levels, derived water level products and datums, and water currents to carry out field operations in support of hydrographic surveying and mapping activities. The hydrographer is concerned not only with the elevation of the sea surface, which is affected significantly by tides, but also with the elevation of lake and river surfaces, where tidal phenomena may have little effect. The term ‘tide’ is traditionally accepted and widely used by hydrographers in connection with the instrumentation used to measure the elevation of the water surface, though the term ‘water level’ would be more technically correct. The term ‘current’ similarly is accepted in many areas in connection with tidal currents; however water currents are greatly affected by much more than the tide producing forces. The term ‘flow’ is often used instead of currents. Tidal forces play such a significant role in completing most hydrographic surveys that tide producing forces and fundamental tidal variations are only described in general with appropriate technical references in this chapter. It is important for the hydrographer to understand why tide, water level and water current characteristics vary both over time and spatially so that they are taken fully into account for survey planning and operations which will lead to successful production of accurate surveys and charts. Because procedures and approaches to measuring and applying water levels, tides and currents vary depending upon the country, this chapter covers general principles using documented examples as appropriate for illustration. -
NSF 03-021, Arctic Research in the United States
This document has been archived. Home is Where the Habitat is An Ecosystem Foundation for Wildlife Distribution and Behavior This article was prepared The lands and near-shore waters of Alaska remaining from recent geomorphic activities such by Page Spencer, stretch from 48° to 68° north latitude and from 130° as glaciers, floods, and volcanic eruptions.* National Park Service, west to 175° east longitude. The immense size of Ecosystems in Alaska are spread out along Anchorage, Alaska; Alaska is frequently portrayed through its super- three major bioclimatic gradients, represented by Gregory Nowacki, USDA Forest Service; Michael imposition on the continental U.S., stretching from the factors of climate (temperature and precipita- Fleming, U.S. Geological Georgia to California and from Minnesota to tion), vegetation (forested to non-forested), and Survey; Terry Brock, Texas. Within Alaska’s broad geographic extent disturbance regime. When the 32 ecoregions are USDA Forest Service there are widely diverse ecosystems, including arrayed along these gradients, eight large group- (retired); and Torre Arctic deserts, rainforests, boreal forests, alpine ings, or ecological divisions, emerge. In this paper Jorgenson, ABR, Inc. tundra, and impenetrable shrub thickets. This land we describe the eight ecological divisions, with is shaped by storms and waves driven across 8000 details from their component ecoregions and rep- miles of the Pacific Ocean, by huge river systems, resentative photos. by wildfire and permafrost, by volcanoes in the Ecosystem structures and environmental Ring of Fire where the Pacific plate dives beneath processes largely dictate the distribution and the North American plate, by frequent earth- behavior of wildlife species. -
Sockeye Salmon Smolt Studies, Kasilof River, Alaska, 1984
SOCKEYE SALMON SMOLT STUDIES KASILOF RIVER, ALASKA 1984 by Loren B. Flagg, Patrick Shields, and David C. Waite Number 47 SOCKEYE SALMON SMOLT STUDIES KASILOF RIVER, ALASKA 1984 Loren B. Flagg, Patrick Shields, and David C. Waite Number 47 Alaska Department of Fish and Game Division of Fisheries Rehabilitation, Enhancement and Development Don W. Collinsworth Commissioner Stanley A. Moberly Director P.O. Box 3-2000 Juneau, Alaska 99802 May 1985 TABLE OF CONTENTS Page ABSTRACT .............................................. 1 INTRODUCTION ........................................ 2 MATERIALS AND METHODS ................................. 4 Fan-Trap and Live-Box Design ..................... 4 Smolt Sampling and Enumeration ................... 5 Smolt Population Estimate ........................ 5 Hatchery Contribution and Survival Rate .......... 7 Physical Parameters .............................. 7 RESULTS ........................................ 8 Smolt Enumeration and Sampling ................... 8 Smolt Population Estimate ........................ 15 Hatchery Contribution and Survival Rate .......... 21 Physical Parameters .............................. 25 Kasilof River Discharge ..................... 25 Water Temperature ........................... 25 DISCUSSION ........................................ 28 ACKNOWLEDGEMENTS ....................................... 34 REFERENCES ........................................ 35 APPENDIX A ............................................ 38 LIST OF TABLES Table Page 1 Daily catches of sockeye salmon -
Pacific Ocean: Supplementary Materials
CHAPTER S10 Pacific Ocean: Supplementary Materials FIGURE S10.1 Pacific Ocean: mean surface geostrophic circulation with the current systems described in this text. Mean surface height (cm) relative to a zero global mean height, based on surface drifters, satellite altimetry, and hydrographic data. (NGCUC ¼ New Guinea Coastal Undercurrent and SECC ¼ South Equatorial Countercurrent). Data from Niiler, Maximenko, and McWilliams (2003). 1 2 S10. PACIFIC OCEAN: SUPPLEMENTARY MATERIALS À FIGURE S10.2 Annual mean winds. (a) Wind stress (N/m2) (vectors) and wind-stress curl (Â10 7 N/m3) (color), multiplied by À1 in the Southern Hemisphere. (b) Sverdrup transport (Sv), where blue is clockwise and yellow-red is counterclockwise circulation. Data from NCEP reanalysis (Kalnay et al.,1996). S10. PACIFIC OCEAN: SUPPLEMENTARY MATERIALS 3 (a) STFZ SAFZ PF 0 100 5.5 17 200 18 16 6 5 4 9 4.5 13 12 15 14 Potential 300 11 10 temperature Depth (m) 6.5 400 9 (°C) 8 7 3.5 500 8 Subtropical Domain Transition Zone Subarctic Domain Alaskan STFZ SAFZ Stream (b) 0 35.2 34.6 34 33 32.7 32.8 100 33.7 33.8 200 34.5 34.3 300 34 34.2 33.9 Depth (m) 34.1 400 34 34.1 Salinity 500 (c) 30°N 40°N 50°N 0 100 2 1 4 8 6 200 10 20 12 14 16 44 25 44 30 300 12 14 35 Depth (m) 16 400 20 40 Nitrate (μmol/kg) 500 (d) 30°NLatitude 40°N 50°N 24.0 Sea surface density Nitrate (μmol/kg) 24.5 θ σ 25.0 1 2 25.5 1 10 2 4 12 8 26.0 14 Potential density 10 12 16 16 26.5 20 25 30 40 35 27.0 30°N 40°N 50°N FIGURE S10.3 The subtropical-subarctic transition along 150 W in the central North Pacific (MayeJune, 1984). -
Alaska! Rw’S Fishing
DELUXE CONDOS “95 lbs. 10 oz.” Our condos are two bedrooms, one bath units. All of our condo units are completely equipped with full kitchens, including dishwasher, refrigerator, range, pots, pans, microwave, toaster and television. ALL PACKAGES INCLUDE: Lodging, all fishing gear while guided (rods, reels, bait). ALASKA! Experienced fishing guide with boat. Plus Free two boxes up to one 100 lbs. of your fish vacuum packed and airport ready. FULLY EQUIPPED CUSTOM BOATS May June July Aug. Sept. Oct. KING SALMON & HALIBUT JULY KENAI & KASILOF RIVERS King Salmon 00 $2197. MAY-JULY 00 Silver Salmon $1997. 7 nights lodging, 3 Salmon fishing trips, and 2 Halibut fishing trips, guided. Pink Salmon SPECIAL FLY-OUT PACKAGE Red Salmon JUNE JULY AUGUST 00 00 00 Trout/ $2147. $2397. $2147. Dolly Varden Includes: 7 nights lodging, 3 Salmon fishing trips with guide, 1 Halibut fishing trip with guide, Halibut 1 fly-out fishing trip to west side of Cook Inlet. *Large runs of pink salmon come on even numbered years. RW’S GUIDED ANGLER www.rwfishing.com BIG EDDY RESORT BIG EDDY 00 SILVER SALMON & HALIBUT $1997. A BY EVER CAUGHT HOME OF THE WORLD’S AUGUST - SEPTEMBER 00 SALMON LARGEST $1997. FISHING Kenai River WE CAN ARRANGE FOR: 7 nights lodging, 3 Salmon fishing trips, and 2 Halibut fishing trips, guided. • Your fishing license • Custom smoking and processing All prices are quoted per person for a party of four. of your catch All packages Sunday thru Saturday. • Mounting of your trophy fish by 1000 Feet of Private River Bank top quality taxidermist Daily Trip Rates Not Included in Packages • Fly outs and other customized trips requested by you 00 King Salmon Charters - May thru July $275. -
Geology of the Prince William Sound and Kenai Peninsula Region, Alaska
Geology of the Prince William Sound and Kenai Peninsula Region, Alaska Including the Kenai, Seldovia, Seward, Blying Sound, Cordova, and Middleton Island 1:250,000-scale quadrangles By Frederic H. Wilson and Chad P. Hults Pamphlet to accompany Scientific Investigations Map 3110 View looking east down Harriman Fiord at Serpentine Glacier and Mount Gilbert. (photograph by M.L. Miller) 2012 U.S. Department of the Interior U.S. Geological Survey Contents Abstract ..........................................................................................................................................................1 Introduction ....................................................................................................................................................1 Geographic, Physiographic, and Geologic Framework ..........................................................................1 Description of Map Units .............................................................................................................................3 Unconsolidated deposits ....................................................................................................................3 Surficial deposits ........................................................................................................................3 Rock Units West of the Border Ranges Fault System ....................................................................5 Bedded rocks ...............................................................................................................................5 -
Geological Characteristics in Cook Inlet Area, Alaska
SOCIE?I’YOF PETROLEUMENGINEERSOF AIME 6200 North CentralExpressway *R SPE 1588 Dallas,Texas 752C6 THIS IS A PREPRINT--- SUBJECTTO CORRECTION Geological Characteristics in Cook Inlet Area, Alaska Downloaded from http://onepetro.org/SPEATCE/proceedings-pdf/66FM/All-66FM/SPE-1588-MS/2087697/spe-1588-ms.pdf by guest on 25 September 2021 By ThomasE. Kelly,Jr. MemberAIYE, Mickl T. Halbouty,Houston,Tex. @ Copyright 19G6 Americsn Institute of Mining, Metallurgical and Petroleum Engineers, Inc. This paper was preparedfor the 41st AnnualFall Meetingof the Societyof PetroleumEngineers of AIME, to be held in Dallas,l?ex.,Oct. 2-5, 1966. permissionto copy is restrictedto an abstract of not more than 300 words. Illustrationsmay not be copied. The abstractshouldcontainconspicu- ous acknowledgmentof whereand by whom the paper is presented. Publicationelsewhereafter publica- tion in the JOURNALOF l?i’TROI.WJMTECHNOLOGYor the SOCIETYOF PETROLEUMENGINEERSJOURNALis usually grantedupon requestto the Editorof the appropriatejournalprovideciagreementto give propercredit is made. Discussionof this paper is invited. Three copiesof any discussionshouldbe sent to the Societyof PetroleumEngineersoffice. Such discussionmay be presentedat the abovemeetingand, with the paper,may be consideredfor publicationin one of the two WE magazines. v, The Cook Inlet basin is a narrow, Although the general characteristics elongate trough of Mesozoic and Ter- of the basin are fairly well known, tiary sediments located north of new information, as it is made avail- latitude 59° in south-central Alaska able will cause many revisions of the (Fig. 1). The basin covers approxi- stratigraphic and structural fabric mately 11,000 square miles of th~ before a complete geological picture northerripart of the Matanuska geo- is possible. -
Chapter 9 Tides and Tidal Currents
CHAPTER 9 TIDES AND TIDAL CURRENTS ORIGINS OF TIDES 900. Introduction superimposed upon non-tidal currents such as normal river flows, floods, and freshets. Tides are the periodic motion of the waters of the sea due to changes in the attractive forces of the Moon and Sun 902. Causes of Tides upon the rotating Earth. Tides can either help or hinder a mariner. A high tide may provide enough depth to clear a The principal tidal forces are generated by the Moon bar, while a low tide may prevent entering or leaving a and Sun. The Moon is the main tide-generating body. Due harbor. Tidal current may help progress or hinder it, may set to its greater distance, the Sun’s effect is only 46 percent of the ship toward dangers or away from them. By the Moon’s. Observed tides will differ considerably from understanding tides and making intelligent use of the tides predicted by equilibrium theory since size, depth, predictions published in tide and tidal current tables and and configuration of the basin or waterway, friction, land descriptions in sailing directions, the navigator can plan an masses, inertia of water masses, Coriolis acceleration, and expeditious and safe passage through tidal waters. other factors are neglected in this theory. Nevertheless, equilibrium theory is sufficient to describe the magnitude 901. Tide and Current and distribution of the main tide-generating forces across The rise and fall of tide is accompanied by horizontal the surface of the Earth. movement of the water called tidal current. It is necessary Newton’s universal law of gravitation governs both the to distinguish clearly between tide and tidal current, for the orbits of celestial bodies and the tide-generating forces relation between them is complex and variable. -
1983 Sport Fishing
LICENSE FEES 1983 Licenses may be purchased from any Alaska Department of Revenue Field Office, or from Department of Revenue license agents (most sporting good stores) throughout the state, or by Al ASKA 1 mail from the Department of Revenue, Fish and Game Licensing, 11 07 W. 8th SI., Juneau, AK 99801 , telephone (907) 465-2376. SPORT FISHING RESIDENT LICENSE REGULA Tl ONS Resident sport fishing license . .. $10 Resident sport fishing license for the blind . 25' SUMMARY Resident hunting and sport fishing license . .$22 Resident hunting, trapping and sport fishing license . $25 Alaska Board of Fisheries However, the fee is 25 cents for the head of a family or a depen Beaton, Jim, Chairman . Juneau dent member of his family or one solely dependent upon himself Sundberg, Harry, Vice Chairman . Wrangel! for support upon proof presented by the applicant thal the appli Angason, Val. .. .. .. ... Dillingham cant: Goessel, Ron .. ... ... .. Stevens Village (A) is obtaining or has obtained assistance during the lsleib, Pete . Cordova 1 preceding six months under any state or federal welfare program Jolin, Ron . Kodiak to aid the indigent, or Weiler, Paul. .. .... Kenai (B) has an annual family gross incarne of less than $5,600 for the year preceding application. Alaska Department of Fish and Game NONRESIDENT LICENSE P.O. Box 3-2000 Visitor's 14-day sport fishing license .. ... $20 Juneau, Alaska 99802 Visitor's three-day sport fishing license . ... $10 Nonresident sport fishing license . $36 Commissioner Nonresident hunting and sport fishing license . $96 Don W. Collinsworth MILITARY LICENSE (on active duty, permanent/y stationed in Alaska) Dlrector, Division of Sport Fish Military sport fishing license .