Definition of IPHC Statistical Areas
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Technical Report No. 70
FISHERIES RESEARCH BOARD OF CANADA TECHNICAL REPORT NO. 70 1968 FISHERIES RESEARCH BOARD OF CANADA Technical Reports FRE Technical Reports are research documents that are of sufficient importance to be preserved, but which for some reason are not aopropriate for scientific pUblication. No restriction is 91aced on subject matter and the series should reflect the broad research interests of FRB. These Reports can be cited in pUblications, but care should be taken to indicate their manuscript status. Some of the material in these Reports will eventually aopear in scientific pUblication. Inquiries concerning any particular Report should be directed to the issuing FRS establishment which is indicated on the title page. FISHERIES RESEARCH BOARD DF CANADA TECHNICAL REPORT NO. 70 Some Oceanographic Features of the Waters of the Central British Columbia Coast by A.J. Dodimead and R.H. Herlinveaux FISHERIES RESEARCH BOARD OF CANADA Biological Station, Nanaimo, B. C. Paci fie Oceanographic Group July 1%6 OONInlTS Page I. INTHOOOCTION II. OCEANOGRAPHIC PlDGRAM, pooa;OORES AND FACILITIES I. Program and procedures, 1963 2. Program and procedures, 1964 2 3. Program and procedures, 1965 3 4 III. GENERAL CHARACICRISTICS OF THE REGION I. Physical characteristics (a) Burke Channel 4 (b) Dean Channel 4 (e) Fi sher Channel and Fitz Hugh Sound 5 2. Climatological features 5 (aJ PrectpitaUon 5 (b) Air temperature 5 (e) Winds 6 (d) Runoff 6 3. Tides 6 4. Oceanographic characteristics 7 7 (a) Burke and Labouchere Channels (i) Upper regime 8 8 (a) Salinity and temperature 8 (b) OJrrents 11 North Bentinck Arm 12 Junction of North and South Bentinck Arms 13 Labouchere Channel 14 (ii) Middle regime 14 (aJ Salinity and temperature (b) OJrrents 14 (iii) Lower regime 14 (aJ 15 Salinity and temperature 15 (bJ OJrrents 15 (bJ Fitz Hugh Sound 16 (a) Salinlty and temperature (bJ CUrrents 16 (e) Nalau Passage 17 (dJ Fi sher Channel 17 18 IV. -
Miles, A.K., M.A. Ricca, R.G. Anthony, and J.A. Estes. 2009
Environmental Toxicology and Chemistry, Vol. 28, No. 8, pp. 1643–1654, 2009 ᭧ 2009 SETAC Printed in the USA 0730-7268/09 $12.00 ϩ .00 ORGANOCHLORINE CONTAMINANTS IN FISHES FROM COASTAL WATERS WEST OF AMUKTA PASS, ALEUTIAN ISLANDS, ALASKA, USA A. KEITH MILES,*† MARK A. RICCA,† ROBERT G. ANTHONY,‡ and JAMES A. ESTES§ †U.S. Geological Survey, Western Ecological Research Center, Davis Field Station, 1 Shields Avenue, University of California, Davis, California 95616 ‡U.S. Geological Survey, Oregon Cooperative Fish and Wildlife Research Unit, 104 Nash Hall, Oregon State University, Corvallis, Oregon 97331 §Department of Ecology and Evolutionary Biology, Center for Ocean Health, 100 Schaffer Road, University of California, Santa Cruz, California 95060, USA (Received 2 October 2008; Accepted 6 March 2009) Abstract—Organochlorines were examined in liver and stable isotopes in muscle of fishes from the western Aleutian Islands, Alaska, in relation to islands or locations affected by military occupation. Pacific cod (Gadus macrocephalus), Pacific halibut (Hippoglossus stenolepis), and rock greenling (Hexagrammos lagocephalus) were collected from nearshore waters at contemporary (decommissioned) and historical (World War II) military locations, as well as at reference locations. Total (⌺) polychlorinated biphenyls (PCBs) dominated the suite of organochlorine groups (⌺DDTs, ⌺chlordane cyclodienes, ⌺other cyclodienes, and ⌺chlo- rinated benzenes and cyclohexanes) detected in fishes at all locations, followed by ⌺DDTs and ⌺chlordanes; dichlorodiphenyldi- chloroethylene (p,pЈDDE) composed 52 to 66% of ⌺DDTs by species. Organochlorine concentrations were higher or similar in cod compared to halibut and lowest in greenling; they were among the highest for fishes in Arctic or near Arctic waters. Organ- ochlorine group concentrations varied among species and locations, but ⌺PCB concentrations in all species were consistently higher at military locations than at reference locations. -
Aleutians PPOR Map 02
Center of map at 54˚ 11.10’ N Lat., 162˚ 59.63’ W Lon. GRS GRS AEA-16 AEA-12 King 35-LII Cove BERING SEA 38-LII Moffet Pt. GRS AEA-15 Amak Is. Cold Bay Kudiakof Islands GRS AEA-16 GRS GRS Fox Is. 37-LII AEA-11 Deer AEA-14 35-LIIGRS38-LII Island AEA-15Cold 36-LII Bay Volcano GRS Bay AEA-14 5 nm 5 nm 5 mi. 5 mi. GRS 5,000 yds. Scale 5,000 yds. Scale Morzhovoi Bay 05-D 57-LI AEA-12 56-LI Cold Bay. Fox Island. King 39-LII Cove False Pass 5 nm GRS GRS 5 mi. 37-LII AEA-11 AEA-12 58-LI Fox Is. 5,000 yds. Scale for Aleutians Subarea Deer False 58-LI Island Pass 57-LI Ikatan Bay Unimak Island Ikatan Bay 03-D 56-LI 03-D 04-D King Cove Otter Cove Unimak Bight (1 nm South) 39-LII 04-D 0.25 nm 0.25 mi. Otter Cove 250 yds. Scale Sanak Island King Cove. False Pass, Otter Cove and Ikatan Bay. 2 nm 2 mi. 2,000 yds. Scale 20 nm r 20 mi. Scale Aleutian Subarea 20,000 yds. Mao p This is not intended for navigational use. Soundings in fathoms t 36-LII a GRS Anchorage # Existing GRS Volcano Bay A# Map c Mooring Fish Hatchery M# Aleutian PPOR o Dock/pier Private Cabins D# L Crane Public Use Cabins Map 02 Volcano Bay. Airport Boat Harbor Legend Potential Places of Refuge Potential NUKA Research & Planning Group, LLC. -
Alaska Tideland Surveys
Alaska Tideland Surveys “Who, What, When, Where, How, Why” A Paper Presented at the th 37 Annual Alaska Surveying and Mapping Conference By Gerald Jennings, P.L.S., and Joe Kemmerer, P.L.S. February, 2002 State of Alaska Department of Natural Resources Division of Mining, Land and Water, Technical and Data Management 550 West 7th Ave, Suite 650 Anchorage, Alaska 99501-3576 (907) 269-8523 Fax (907) 269-8914 ii ABSTRACT Alaska Tideland Surveys – the 5 w’s. Surveys of tideland parcels are unique in several ways. Typically all corners are monumented with witness corners. DNR is usually the fee owner of the parcel, and the landward boundary is usually the mean high water line. Frequently, the line is fixed and limiting, because of avulsion, or placement of fill. This paper will briefly discuss how an applicant applies for a tideland lease or conveyance and how to conduct the survey and obtain state approval. Presenter: Gerald Jennings The Department of Natural Resources, Division of Mining, Land and Water, Technical and Data Management staff dealing with Alaska Tideland Surveys: Gerald Jennings, P.L.S., Statewide Platting Supervisor Joe Kemmerer, P.L.S., Coastal Boundary. William (Bill) Brown, P.L.S., Riparian Specialist iii Alaska Tideland Surveys Introduction – who what why? Title to most of the tide and submerged lands surrounding Alaska was vested in the State of Alaska under the Submerged Lands Act of May 22, 1953. Most of those lands remain in state ownership and in most cases, the state will lease, but retain fee title. As a surveyor, you will be contacted about Alaska Tideland Surveys (ATS) by a public or private party who desires to lease or acquire tidelands for various reasons such as construction of docks, bridges, harbors, log transfer facilities, etc. -
British Columbia Regional Guide Cat
National Marine Weather Guide British Columbia Regional Guide Cat. No. En56-240/3-2015E-PDF 978-1-100-25953-6 Terms of Usage Information contained in this publication or product may be reproduced, in part or in whole, and by any means, for personal or public non-commercial purposes, without charge or further permission, unless otherwise specified. You are asked to: • Exercise due diligence in ensuring the accuracy of the materials reproduced; • Indicate both the complete title of the materials reproduced, as well as the author organization; and • Indicate that the reproduction is a copy of an official work that is published by the Government of Canada and that the reproduction has not been produced in affiliation with or with the endorsement of the Government of Canada. Commercial reproduction and distribution is prohibited except with written permission from the author. For more information, please contact Environment Canada’s Inquiry Centre at 1-800-668-6767 (in Canada only) or 819-997-2800 or email to [email protected]. Disclaimer: Her Majesty is not responsible for the accuracy or completeness of the information contained in the reproduced material. Her Majesty shall at all times be indemnified and held harmless against any and all claims whatsoever arising out of negligence or other fault in the use of the information contained in this publication or product. Photo credits Cover Left: Chris Gibbons Cover Center: Chris Gibbons Cover Right: Ed Goski Page I: Ed Goski Page II: top left - Chris Gibbons, top right - Matt MacDonald, bottom - André Besson Page VI: Chris Gibbons Page 1: Chris Gibbons Page 5: Lisa West Page 8: Matt MacDonald Page 13: André Besson Page 15: Chris Gibbons Page 42: Lisa West Page 49: Chris Gibbons Page 119: Lisa West Page 138: Matt MacDonald Page 142: Matt MacDonald Acknowledgments Without the works of Owen Lange, this chapter would not have been possible. -
Fishery Circular
NOAA TR NMFS CIRC-383 A UNITED STATES DEPARTMENT OF COMMERCE PUBLICATION NOAA Technical Report NMFS CI RC-383 twm fiioloHar uooriwy / **- \ U.S. DEPARTMENT OF COMMERCE , I- Q , V National Oceanic and Atmospheric Administration %, 't' (^ National Marine Fisheries Service \ 1 J- L Fishery Publications, Calendar Year 1965: Lists and Indexes LEE C. THORSON and MARY ELLEN ENGETT SEATTLE, WA JULY 1973 NOAA TECHNICAL REPORTS National Marine Fisheries Service, Circulars The major responsibilities of the National Marine Fisheries Ser\-ice (NMFS) are to monitor and assess the abundance and geographic distribution of fishery resources, to understand and predict fluctuations in the quan- tity and distribution of these resources, and to establish levels for optimum use of the resources. NMFS is also charged with the development and implementation of policies for managing national fishing grounds, develop- ment and enforcement of domestic fisheries regulations, surveillance of foreign fishing off United States coastal waters, and the development and enforcement of international fishery agreements and policies. NMFS also assists the fishing industry through marketing service and economic analysis programs, and mortgage insurance and vessel construction subsidies. It collects, analyses, and publishes statistics on various phases of the industry. The NOA.\ Technical Report NMFS CIRC series continues a series that has been in e.xistence since 1941. The Circulars are technical publications of general interest intended to aid conservation and management. Publica- tions that review in considerable detail and at a high technical level certain broad areas of research appear in this series. Technical papers originating in economics studies and from management investigations appear in the Circular series. -
Long-Term Measurements of Flow Near the Aleutian Islands
Journal of Marine Research, 55,565-575,1997 Long-term measurements of flow near the Aleutian Islands by R. K. Reed’ and P. J. Stabenol ABSTRACT In summer1995, the AlaskanStream at 173.5Wwas very intense;the peakgeostrophic speed was -125 cm s-l, and the computedvolume transportabove 1000db, referred to 1000db, was 9 X lo6 m3s-l. Flow north of the central Aleutians was shallow, convoluted and weak (2- 3 X lo6 m3SK’). A sequenceof CTD castsacross Amukta Pass,spaced irregularly in time during 1993-1996,showed a meannorthward (southward) geostrophic transport of 1.0 (0.4) X lo6 m3s-t, for a net flow into the Bering Seaof 0.6 X lo6 m3s-t. The sourceof this flow wasthe Alaskan Stream exceptin 1995,when it wasBering Sea water. Results from two 13-monthcurrent mooringswest and eastof the passwere quite different.To the west,flow wasweak andvariable and appeared to have a barotropiccomponent. To the east,flow wasstronger and unidirectional eastward. 1. Introduction Upper-ocean circulation near the central Aleutian Islands is characterized by the swift, westward flowing Alaskan Stream on the southern side and by a relatively weak, eastward flow on the northern side (Favorite, 1974; Sayles et al., 1979). There is exchange between thesetwo flows, however, through the two deep passesacross the ridge near 180 and 172W (Reed and Stabeno, 1994). One of our objectives was to obtain frequent samplesof the density field acrossthe passnear 172W (Amukta Pass; Fig. l), primarily becauseit is a pathway for relatively warm (>4”C) Alaskan Stream water into the Bering Sea (Reed, 1995). -
Aleutian Islands
Journal of Global Change Data & Discovery. 2018, 2(1): 109-114 © 2018 GCdataPR DOI:10.3974/geodp.2018.01.18 Global Change Research Data Publishing & Repository www.geodoi.ac.cn Global Change Data Encyclopedia Aleutian Islands Liu, C.1* Yang, A. Q.2 Hu, W. Y.1 Liu, R. G.1 Shi, R. X.1 1. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 2. Institute of Remote Sensing and Digital Earth,Chinese Academy of Sciences,Beijing100101,China Keywords: Aleutian Islands; Fox Islands; Four Mountains Islands; Andreanof Islands; Rat Islands; Near Islands; Kommandor Islands; Unimak Island; USA; Russia; data encyclopedia The Aleutian Islands extends latitude from 51°12′35″N to 55°22′14″N and longitude about 32 degrees from 165°45′10″E to 162°21′10″W, it is a chain volcanic islands belonging to both the United States and Russia[1–3] (Figure 1, 2). The islands are formed in the northern part of the Pacific Ring of Fire. They form part of the Aleutian Arc in the Northern Pacific Ocean, extending about 1,900 km westward from the Alaska Peninsula to- ward the Kamchatka Peninsula in Russia, Figure 1 Dataset of Aleutian Islands in .kmz format and mark a dividing line between the Ber- ing Sea to the north and the Pacific Ocean to the south. The islands comprise 6 groups of islands (east to west): the Fox Islands[4–5], islands of Four Mountains[6–7], Andreanof Islands[8–9], Rat Islands[10–11], Near Is- lands[12–13] and Kommandor Islands[14–15]. -
Southeast Alaska Mid-Region Access Port and Ferry Terminal Technical Memorandum
S A M-R A P Ferr T T M Prepared for Fr Highw An Through R Pecci Associates, I. 825 Custer Avenue Helena, Montana 59604 (406)447-5000 www.rpa-hln.com Prepared by T Gos Associates, I. 1201 Western Avenue, Suite 200 Seattle, WA 98101 www.glosten.com Pametri, I. 700 NE Multnomah, Suite 1000 Portland, OR 97232-4110 T. 503.233.2400 F, 503.233.4825 www.parametrix.com CITATION The Glosten Associates, Inc., Parametrix, Inc. 2011. Southeast Alaska Mid-Region Access Port and Ferry Terminal Technical Memorandum. Prepared by The Glosten Associates, Inc., Seattle, Washington, Parametrix, Inc., Portland, Oregon. April 2011. Port and Ferry Terminal Technical Memorandum TABLE OF CONTENTS EXECUTIVE SUMMARY ....................................................................................................... ES-1 1 INTRODUCTION ................................................................................................................ 1-1 1.1 Purpose of the Mid-Region Access Study ......................................................................... 1-1 1.2 Southeast Alaska Mid-Region Access Study Corridors ..................................................... 1-3 1.2.1 Bradfield Canal Corridor ....................................................................................... 1-3 1.2.2 Stikine River Corridor ........................................................................................... 1-5 1.2.3 Aaron Creek Corridor............................................................................................ 1-5 1.3 Characteristics -
Final 2012 NHLPA Report Noapxb.Pub
GSA Office of Real Property Utilization and Disposal 2012 PROGRAM HIGHLIGHTS REPORT NATIONAL HISTORIC LIGHTHOUSE PRESERVATION ACT EXECUTIVE SUMMARY Lighthouses have played an important role in America’s For More Information history, serving as navigational aids as well as symbols of our rich cultural past. Congress passed the National Information about specific light stations in the Historic Lighthouse Preservation Act (NHLPA) in 2000 to NHLPA program is available in the appendices and establish a lighthouse preservation program that at the following websites: recognizes the cultural, recreational, and educational National Park Service Lighthouse Heritage: value of these iconic properties, especially for local http://www.nps.gov/history/maritime/lt_index.htm coastal communities and nonprofit organizations as stewards of maritime history. National Park Service Inventory of Historic Light Stations: http://www.nps.gov/maritime/ltsum.htm Under the NHLPA, historic lighthouses and light stations (lights) are made available for transfer at no cost to Federal agencies, state and local governments, and non-profit organizations (i.e., stewardship transfers). The NHLPA Progress To Date: NHLPA program brings a significant and meaningful opportunity to local communities to preserve their Since the NHLPA program’s inception in 2000, 92 lights maritime heritage. The program also provides have been transferred to eligible entities. Sixty-five substantial cost savings to the United States Coast percent of the transferred lights (60 lights) have been Guard (USCG) since the historic structures, expensive to conveyed through stewardship transfers to interested repair and maintain, are no longer needed by the USCG government or not-for-profit organizations, while 35 to meet its mission as aids to navigation. -
Preliminary Reconnaissance Geologic Map of the Petersburg and Parts of the Port Alexander and Sumdum 1:250,000 Quadrangles, Southeastern Alaska
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Preliminary reconnaissance geologic map of the Petersburg and parts of the Port Alexander and Sumdum 1:250,000 quadrangles, southeastern Alaska By David A. Brew , A. Thomas Ovenshine , Susan M. Karl , and Susan J. Hunt* Open-File Report 84-405 This report is preliminary and has not been reviewed for conformity with U.S Geological Survey editorial standards and strati graphic nomenclature. *Menlo Park, California ^Reston, Virginia ^Anchorage, Alaska Preliminary reconnaissance geologic map of the Petersburg and parts of the Port Alexander and Sumdum 1:250,000 quadrangles, southeastern Alaska By David A. Brew, A. T. Ovenshine, Susan M. Karl, and Susan J. Hunt INTRODUCTION This report consists of three main items: (1) the geologic map (sheet 1 of 2), (2) the correlation of map units (sheet 2 of 2), which includes an inset map relating different parts of the map to the correlation of map units and to (3) the description of map units (this pamphlet). The inset map on sheet 2 shows the major geological elements of the map area. They are, from west to east, (1) the Alexander belt, consisting of generally unmetamorphosed Lower Paleozoic through Upper Triassic rocks intruded by scattered mid-Cretaceous plutons, (2) the Gravina belt, consisting of unmetamorphosed to highly metamorphosed, variably deformed Upper Jurassic(?) through mid-Cretaceous flysch and volcanic rocks intruded by both mid- and Upper Cretaceous plutons, and (3) the Mainland belt, consisting of metamorphic rocks intruded by Upper Cretaceous, lower Tertiary, and mid- Tertiary plutons. Younger than almost all parts of all of these belts, and extending from the Alexander belt across the Gravina and onto the mainland belt, is the lower to middle Tertiary Kuiu-Etolin belt that consists largely of varied volcanic rocks, associated plutons, and minor sedimentary rocks. -
North Pacific Internal Tides from the Aleutian Ridge
Journalof Marine Research, 59, 167–191, 2001 Journal of MARINE RESEARCH Volume59, Number 2 NorthPaci c internaltides fromthe Aleutian Ridge: Altimeterobservations andmodeling byPatrickF. Cummins 1,JosefY. Cherniawsky 1 andMichael G. G.Foreman 1 ABSTRACT Internaltides radiating into the North Paci c fromthe Aleutian Ridge near Amukta Pass are examinedusing 7 yearsof Topex/ Poseidonaltimeter data. The observations show coherent southwardphase propagation at the M2 frequencyover a distanceof atleast1100 km intothe central Pacic. Barotropicand baroclinic models are applied to study this internal tidal signal. Results from thebarotropic model show that the strongest cross-slope volume and energy uxesoccur in the vicinityof Amukta Pass, helping to establish this region as an important site for baroclinic energy conversionalong the eastern half of theridge. Atwo-dimensionalversion of the Princeton Ocean Model is used to simulate internal tide generationand propagation. A comparisonbetween the altimeter data south of the ridge and the sea-surfacesignature of theinternal tide signal of the model shows good agreement for the phase, bothclose to thesourceand well into the far eld.Comparison of thephase between model and data alsoprovides evidence for wave refraction. This occurs due to the slow modulation of wavelength associatedwith the variation in the Coriolis parameter encountered as the internal tide propagates southward.The model results suggest that the net rate of conversion of barotropic to baroclinic energyis about 1.8 GW inthe vicinity of Amukta Pass. This represents about 6% of the local barotropicenergy uxacrossthe ridge and perhaps 1% ofglobalbaroclinic conversion. 1.Introduction Prior tothelaunch of the Topex-Poseidon (T/ P)missionin August,1992, it was widely heldthat oceanic internal tides generally did not propagate more than short distance away from asourceregion before becoming ‘ incoherent,’that is, before losing their phase relationwith the generating surface tide.