Western Birds
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Fronts in the World Ocean's Large Marine Ecosystems. ICES CM 2007
- 1 - This paper can be freely cited without prior reference to the authors International Council ICES CM 2007/D:21 for the Exploration Theme Session D: Comparative Marine Ecosystem of the Sea (ICES) Structure and Function: Descriptors and Characteristics Fronts in the World Ocean’s Large Marine Ecosystems Igor M. Belkin and Peter C. Cornillon Abstract. Oceanic fronts shape marine ecosystems; therefore front mapping and characterization is one of the most important aspects of physical oceanography. Here we report on the first effort to map and describe all major fronts in the World Ocean’s Large Marine Ecosystems (LMEs). Apart from a geographical review, these fronts are classified according to their origin and physical mechanisms that maintain them. This first-ever zero-order pattern of the LME fronts is based on a unique global frontal data base assembled at the University of Rhode Island. Thermal fronts were automatically derived from 12 years (1985-1996) of twice-daily satellite 9-km resolution global AVHRR SST fields with the Cayula-Cornillon front detection algorithm. These frontal maps serve as guidance in using hydrographic data to explore subsurface thermohaline fronts, whose surface thermal signatures have been mapped from space. Our most recent study of chlorophyll fronts in the Northwest Atlantic from high-resolution 1-km data (Belkin and O’Reilly, 2007) revealed a close spatial association between chlorophyll fronts and SST fronts, suggesting causative links between these two types of fronts. Keywords: Fronts; Large Marine Ecosystems; World Ocean; sea surface temperature. Igor M. Belkin: Graduate School of Oceanography, University of Rhode Island, 215 South Ferry Road, Narragansett, Rhode Island 02882, USA [tel.: +1 401 874 6533, fax: +1 874 6728, email: [email protected]]. -
2018 Spring WTC Newsletter
Vol. 29, No. 1 / Spring 2018 Blood, Sweat and Ink on the PCT (pg. 2) Is This the End? (pg. 5) Adventure in Your Own Backyard (pg. 6) Experience Trips: You Want Them, We’ve Got Them! (pg. 12) Shawnté Salabert, guidebook author and WTC instructor, on the Pacific Crest Trail WTC OFFICERS Contents (see your Student Handbook for contact information) WTC Chair WTC Outings Co-Chairs Bob Myers Adrienne Benedict Tom McDonnell WTC Registrar FEATURES Jim Martins LONG BEACH/SOUTH BAY SAN GABRIEL VALLEY Smiles, Not Miles Area Chair Area Chair Writer and WTC-instructor Shawnté Salabert spent 2 Brian Decker Jeremy Netka more than two years writing the guidebook on Area Vice Chair Area Vice Chair section hiking the southern section of the Pacific Sharon Moore Jan Marie Perry Crest Trail—and she’s got some advice for you. Area Trips Area Trips Mike Adams Mat Kelliher Is This the End? Spoiler alert—no, it isn’t! Lubna Debbini and Victor 5 Area Registrar Area Registrar Joan Rosenburg Amy Smith Gomez point you down the road of post-WTC fun and adventure. ORANGE COUNTY WEST LOS ANGELES Area Chair Area Chair Adventure in Your Own Backyard Matt Hengst Pamela Sivula Ditch the long drive—in Southern California 6 Area Vice Chair Area Vice Chair there’s adventure right out the back door and Gary McCoppin Katerina Leong Will McWhinney has a few ideas. Area Trips Area Trips Matt Hengst Adrienne Benedict Alphabet Soup Dig into the Angeles Chapter’s sections and you 8 Area Registrar Area Registrar find plenty of outdoor and other possibilities— Wendy Miller Pamela Sivula and acronyms. -
Contemporary State of Glaciers in Chukotka and Kolyma Highlands ISSN 2080-7686
Bulletin of Geography. Physical Geography Series, No. 19 (2020): 5–18 http://dx.doi.org/10.2478/bgeo-2020-0006 Contemporary state of glaciers in Chukotka and Kolyma highlands ISSN 2080-7686 Maria Ananicheva* 1,a, Yury Kononov 1,b, Egor Belozerov2 1 Russian Academy of Science, Institute of Geography, Moscow, Russia 2 Lomonosov State University, Faculty of Geography, Moscow, Russia * Correspondence: Russian Academy of Science, Institute of Geography, Moscow, Russia. E-mail: [email protected] a https://orcid.org/0000-0002-6377-1852, b https://orcid.org/0000-0002-3117-5554 Abstract. The purpose of this work is to assess the main parameters of the Chukotka and Kolyma glaciers (small forms of glaciation, SFG): their size and volume, and changes therein over time. The point as to whether these SFG can be considered glaciers or are in transition into, for example, rock glaciers is also presented. SFG areas were defined from the early 1980s (data from the catalogue of the glaciers compiled by R.V. Sedov) to 2005, and up to 2017: these data were retrieved from sat- Key words: ellite images. The maximum of the SGF reduction occurred in the Chantalsky Range, Iskaten Range, Chukotka Peninsula, and in the northern part of Chukotka Peninsula. The smallest retreat by this time relates to the gla- Kolyma Highlands, ciers of the southern part of the peninsula. Glacier volumes are determined by the formula of S.A. satellite image, Nikitin for corrie glaciers, based on in-situ volume measurements, and by our own method: the av- climate change, erage glacier thickness is calculated from isogypsum patterns, constructed using DEMs of individu- glacier reduction, al glaciers based on images taken from a drone during field work, and using ArcticDEM for others. -
Arctic Research of the United States, Volume 15
This document has been archived. About The journal Arctic Research of the United refereed for scientific content or merit since the States is for people and organizations interested journal is not intended as a means of reporting the in learning about U.S. Government-financed scientific research. Articles are generally invited Arctic research activities. It is published semi- and are reviewed by agency staffs and others as Journal annually (spring and fall) by the National Science appropriate. Foundation on behalf of the Interagency Arctic As indicated in the U.S. Arctic Research Plan, Research Policy Committee (IARPC) and the research is defined differently by different agencies. Arctic Research Commission (ARC). Both the It may include basic and applied research, moni- Interagency Committee and the Commission were toring efforts, and other information-gathering authorized under the Arctic Research and Policy activities. The definition of Arctic according to Act (ARPA) of 1984 (PL 98-373) and established the ARPA is “all United States and foreign terri- by Executive Order 12501 (January 28, 1985). tory north of the Arctic Circle and all United Publication of the journal has been approved by States territory north and west of the boundary the Office of Management and Budget. formed by the Porcupine, Yukon, and Kuskokwim Arctic Research contains Rivers; all contiguous seas, including the Arctic • Reports on current and planned U.S. Govern- Ocean and the Beaufort, Bering, and Chukchi ment-sponsored research in the Arctic; Seas; and the Aleutian chain.” Areas outside of • Reports of ARC and IARPC meetings; and the boundary are discussed in the journal when • Summaries of other current and planned considered relevant to the broader scope of Arctic Arctic research, including that of the State of research. -
Sources and Pathways 4.1
Chapter 4 Persistant toxic substances (PTS) sources and pathways 4.1. Introduction Chapter 4 4.1. Introduction 4.2. Assessment of distant sources: In general, the human environment is a combination Longrange atmospheric transport of the physical, chemical, biological, social and cultur- Due to the nature of atmospheric circulation, emission al factors that affect human health. It should be recog- sources located within the Northern Hemisphere, par- nized that exposure of humans to PTS can, to certain ticularly those in Europe and Asia, play a dominant extent, be dependant on each of these factors. The pre- role in the contamination of the Arctic. Given the spa- cise role differs depending on the contaminant con- tial distribution of PTS emission sources, and their cerned, however, with respect to human intake, the potential for ‘global’ transport, evaluation of long- chain consisting of ‘source – pathway – biological avail- range atmospheric transport of PTS to the Arctic ability’ applies to all contaminants. Leaving aside the region necessarily involves modeling on the hemi- biological aspect of the problem, this chapter focuses spheric/global scale using a multi-compartment on PTS sources, and their physical transport pathways. approach. To meet these requirements, appropriate modeling tools have been developed. Contaminant sources can be provisionally separated into three categories: Extensive efforts were made in the collection and • Distant sources: Located far from receptor sites in preparation of input data for modeling. This included the Arctic. Contaminants can reach receptor areas the required meteorological and geophysical informa- via air currents, riverine flow, and ocean currents. tion, and data on the physical and chemical properties During their transport, contaminants are affected by of both the selected substances and of their emissions. -
Street Index Listing.Pdf
Mesa County Street INDEX Wednesday, September 26, 2018 8:07:26 AM StreetName Township SuperNbhd Super_NBHD_Description 2431‐281 0 M & B 2691‐242 0 M & B B 1/2 2943‐294 7299 MORSE SUBDIVISION G 2945‐011 2106 Vista Del Norte PEAR MEADOWS 2943‐163 7276 PEAR MEADOWS SUBDIVISION FILING NO 2 10 2683‐101 0 M & B 10 1/2 2691‐071 0 M & B 10TH 2945‐111 2528 Old Capital Hill M&B 11 2683‐141 0 M & B 11 8/10 2691‐053 0 M & B 11TH 2945‐111 2215 Wellington Bus Park 12 2691‐054 2847 Hoelscher II SLD 12 1/2 2691‐093 0 M & B 12 1/4 2691‐333 0 M & B 12 3/4 2691‐331 776 Loma Townsite Vac B33,48,49,64 12 8/10 3749‐021 0 M & B 12TH 2945‐012 0 M & B 13 2691‐091 0 M & B 13 1/2 2693‐032 0 M & B 13 1/8 2691‐343 777 Refiling of the Loma Townsite 13 2/10 2693‐032 3397 Red Canyons Vista II 13 3/10 2691‐273 5022 Elaine SLD 13 3/4 2691‐341 0 M & B 13TH 2945‐013 441 Fairmount North 14 2691‐104 0 M & B 14 1/2 2691‐111 0 M & B 14TH 2945‐013 441 Fairmount North 15 2691‐133 0 M & B 15 1/2 2691‐361 0 M & B 15 3/4 2959‐351 0 M & B 15 3/8 2691‐362 2358 Refinery Heights Page 1 of 83 StreetName Township SuperNbhd Super_NBHD_Description 15TH 2945‐012 1664 Ptarmigan Ridge (all) 16 2435‐231 0 M & B 16 1/10 3469‐141 0 M & B 16 1/2 2697‐061 0 M & B 16TH 2945‐123 1353 Sunnyvale Acres 17 2695‐172 0 M & B 17 1/2 2695‐172 0 M & B 17 1/4 2697‐082 0 M & B 17 3/4 2695‐291 3569 Lucki Estates 17 7/10 2961‐191 0 M & B 17TH 2945‐122 0 M & B 18 2437‐223 0 M & B 18 1/2 2695‐332 3297 Horseshoe Ridge Est #2 18TH 2945‐123 423 Elmwood Plaza Amend 19 2695‐164 2932 Driftwood Farms SLD 19 1/2 2697‐151 -
Flow of Pacific Water in the Western Chukchi
Deep-Sea Research I 105 (2015) 53–73 Contents lists available at ScienceDirect Deep-Sea Research I journal homepage: www.elsevier.com/locate/dsri Flow of pacific water in the western Chukchi Sea: Results from the 2009 RUSALCA expedition Maria N. Pisareva a,n, Robert S. Pickart b, M.A. Spall b, C. Nobre b, D.J. Torres b, G.W.K. Moore c, Terry E. Whitledge d a P.P. Shirshov Institute of Oceanology, 36, Nakhimovski Prospect, Moscow 117997, Russia b Woods Hole Oceanographic Institution, 266 Woods Hole Road, Woods Hole, MA 02543, USA c Department of Physics, University of Toronto, 60 St. George Street, Toronto, Ontario M5S 1A7, Canada d University of Alaska Fairbanks, 505 South Chandalar Drive, Fairbanks, AK 99775, USA article info abstract Article history: The distribution of water masses and their circulation on the western Chukchi Sea shelf are investigated Received 10 March 2015 using shipboard data from the 2009 Russian-American Long Term Census of the Arctic (RUSALCA) pro- Received in revised form gram. Eleven hydrographic/velocity transects were occupied during September of that year, including a 25 August 2015 number of sections in the vicinity of Wrangel Island and Herald canyon, an area with historically few Accepted 25 August 2015 measurements. We focus on four water masses: Alaskan coastal water (ACW), summer Bering Sea water Available online 31 August 2015 (BSW), Siberian coastal water (SCW), and remnant Pacific winter water (RWW). In some respects the Keywords: spatial distributions of these water masses were similar to the patterns found in the historical World Arctic Ocean Ocean Database, but there were significant differences. -
Alpha Codes for 2168 Bird Species (And 113 Non-Species Taxa) in Accordance with the 62Nd AOU Supplement (2021), Sorted Taxonomically
Four-letter (English Name) and Six-letter (Scientific Name) Alpha Codes for 2168 Bird Species (and 113 Non-Species Taxa) in accordance with the 62nd AOU Supplement (2021), sorted taxonomically Prepared by Peter Pyle and David F. DeSante The Institute for Bird Populations www.birdpop.org ENGLISH NAME 4-LETTER CODE SCIENTIFIC NAME 6-LETTER CODE Highland Tinamou HITI Nothocercus bonapartei NOTBON Great Tinamou GRTI Tinamus major TINMAJ Little Tinamou LITI Crypturellus soui CRYSOU Thicket Tinamou THTI Crypturellus cinnamomeus CRYCIN Slaty-breasted Tinamou SBTI Crypturellus boucardi CRYBOU Choco Tinamou CHTI Crypturellus kerriae CRYKER White-faced Whistling-Duck WFWD Dendrocygna viduata DENVID Black-bellied Whistling-Duck BBWD Dendrocygna autumnalis DENAUT West Indian Whistling-Duck WIWD Dendrocygna arborea DENARB Fulvous Whistling-Duck FUWD Dendrocygna bicolor DENBIC Emperor Goose EMGO Anser canagicus ANSCAN Snow Goose SNGO Anser caerulescens ANSCAE + Lesser Snow Goose White-morph LSGW Anser caerulescens caerulescens ANSCCA + Lesser Snow Goose Intermediate-morph LSGI Anser caerulescens caerulescens ANSCCA + Lesser Snow Goose Blue-morph LSGB Anser caerulescens caerulescens ANSCCA + Greater Snow Goose White-morph GSGW Anser caerulescens atlantica ANSCAT + Greater Snow Goose Intermediate-morph GSGI Anser caerulescens atlantica ANSCAT + Greater Snow Goose Blue-morph GSGB Anser caerulescens atlantica ANSCAT + Snow X Ross's Goose Hybrid SRGH Anser caerulescens x rossii ANSCAR + Snow/Ross's Goose SRGO Anser caerulescens/rossii ANSCRO Ross's Goose -
ABSTRACT Title of Dissertation: SECRETIVE MARSHBIRDS of URBAN WETLANDS in the WASHINGTON, DC METROPOLITAN AREA Patrice Nielson
ABSTRACT Title of Dissertation: SECRETIVE MARSHBIRDS OF URBAN WETLANDS IN THE WASHINGTON, DC METROPOLITAN AREA Patrice Nielson, Doctor of Philosophy 2016 Dissertation directed by: Dr. William Bowerman and Dr. Andrew Baldwin Environmental Science and Technology Secretive marshbirds are in decline across their range and are species of greatest conservation need in state Wildlife Action Plans. However, their secretive nature means there is relatively sparse information available on their ecology. There is demand for this information in the Washington, DC area for updating conservation plans and guiding wetland restoration. Rapid Wetland Assessment Methods are often used to monitor success of restoration but it is unknown how well they indicate marshbird habitat. Using the Standardized North American Marshbird Monitoring Protocol, I surveyed 51 points in 25 marshes in the DC area in 2013 – 2015. I also collected data on marsh area, buffer width, vegetation/water interspersion, vegetation characteristics, flooding, and invertebrates. At each bird survey point I assessed wetland quality using the Floristic Quality Assessment Index (FQAI) and California Rapid Wetland Assessment (CRAM) methods. I used Program Presence to model detection and occupancy probabilities of secretive marshbirds as a function of habitat variables. I found king rails (Rallus elegans) at five survey sites and least bittern (Ixobrychus exilis) at thirteen survey sites. Secretive marshbirds were using both restored and natural marshes, marshes with and without invasive plant species, and marshes with a variety of dominant vegetation species. King rail occupancy was positively correlated with plant diversity and invertebrate abundance and weakly negatively correlated with persistent vegetation. Least bittern occupancy was strongly negatively correlated woody vegetation and invertebrate abundance and weakly positively correlated with persistent vegetation. -
Red List of Bangladesh 2015
Red List of Bangladesh Volume 1: Summary Chief National Technical Expert Mohammad Ali Reza Khan Technical Coordinator Mohammad Shahad Mahabub Chowdhury IUCN, International Union for Conservation of Nature Bangladesh Country Office 2015 i The designation of geographical entitles in this book and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of IUCN, International Union for Conservation of Nature concerning the legal status of any country, territory, administration, or concerning the delimitation of its frontiers or boundaries. The biodiversity database and views expressed in this publication are not necessarily reflect those of IUCN, Bangladesh Forest Department and The World Bank. This publication has been made possible because of the funding received from The World Bank through Bangladesh Forest Department to implement the subproject entitled ‘Updating Species Red List of Bangladesh’ under the ‘Strengthening Regional Cooperation for Wildlife Protection (SRCWP)’ Project. Published by: IUCN Bangladesh Country Office Copyright: © 2015 Bangladesh Forest Department and IUCN, International Union for Conservation of Nature and Natural Resources Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holders, provided the source is fully acknowledged. Reproduction of this publication for resale or other commercial purposes is prohibited without prior written permission of the copyright holders. Citation: Of this volume IUCN Bangladesh. 2015. Red List of Bangladesh Volume 1: Summary. IUCN, International Union for Conservation of Nature, Bangladesh Country Office, Dhaka, Bangladesh, pp. xvi+122. ISBN: 978-984-34-0733-7 Publication Assistant: Sheikh Asaduzzaman Design and Printed by: Progressive Printers Pvt. -
Emergency Plan
Environmental Impact Assessment Project Number: 43253-026 November 2019 India: Karnataka Integrated and Sustainable Water Resources Management Investment Program – Project 2 Vijayanagara Channels Annexure 5–9 Prepared by Project Management Unit, Karnataka Integrated and Sustainable Water Resources Management Investment Program Karnataka Neeravari Nigam Ltd. for the Asian Development Bank. This is an updated version of the draft originally posted in June 2019 available on https://www.adb.org/projects/documents/ind-43253-026-eia-0 This environmental impact assessment is a document of the borrower. The views expressed herein do not necessarily represent those of ADB's Board of Directors, Management, or staff, and may be preliminary in nature. Your attention is directed to the “terms of use” section on ADB’s website. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a particular territory or geographic area in this document, the Asian Development Bank does not intend to make any judgments as to the legal or other status of any territory or area. Annexure 5 Implementation Plan PROGRAMME CHART FOR CANAL LINING, STRUCTURES & BUILDING WORKS Name Of the project:Modernization of Vijaya Nagara channel and distributaries Nov-18 Dec-18 Jan-19 Feb-19 Mar-19 Apr-19 May-19 Jun-19 Jul-19 Aug-19 Sep-19 Oct-19 Nov-19 Dec-19 Jan-20 Feb-20 Mar-20 Apr-20 May-20 Jun-20 Jul-20 Aug-20 Sep-20 Oct-20 Nov-20 Dec-20 S. No Name of the Channel 121212121212121212121212121212121212121212121212121 2 PACKAGE -
Treeline Dynamics on Southern Vancouver Island, British Columbia
Western Geography, 10/11(2000/01), pp. 43–63 ©Western Division, Canadian Association of Geographers Treeline Dynamics on Southern Vancouver Island, British Columbia Colin P. Laroque, David H. Lewis and Dan J. Smith* Department of Geography—Ring Laboratory University of Victoria Victoria, BC V8W 3P5 This paper describes the nature of treeline dynamics and upper-elevation tree establishment patterns on southern Vancouver Island, British Columbia. We examined tree growth, climate and seedling relationships at three upper-elevation locations using standard dendroecolog- ical approaches. Our data suggest that this habitat has experienced species-specific pulses of tree establishment that have had a major impact on the character of the local treeline boundaries. The stem data collected within quadrats at Gemini Mountain and Haley Bowl show that seedling establishment within the last three cen- turies was episodic and linked to historical climatic pat- terns. Successful mountain hemlock establishment in this setting is restricted to periods characterized by either cool summers and shallow winter snowpacks, or warmer than normal summers and moderately deep snowpacks. The establishment of amabilis and subalpine fir seedlings appears restricted to intervals with cool growing seasons and moderately deep seasonal snow- packs. Episodic seedling establishment in the 20th cen- tury has resulted in a gradual infilling of the local tree- line and the development of a more structured parkland belt that is expected to have habitat implications for endangered Vancouver Island marmot. Keywords: dendroecology, subalpine meadows, seedling establishment, tree rings, Vancouver Island, Vancouver Island marmot. *Corresponding author 44 Laroque, Lewis & Smith Introduction Little is known of the nature of long-term treeline dynamics on Vancouver Island.