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F!L3ljnew CITATIONS in COASTAL TOPICS • a
·/f1!f!!II:. f!l3lJNEW CITATIONS IN COASTAL TOPICS • A ., Addis, R.P.; Garstand, M., and Emmitt, G.D., J9R4. Downdrafts from tropical oceanic cumuli. Boundary-Layer Meteorology. 28(1-2).23-49. Admiraal, W.; Laane, R.W.P.M., and Peletier, H., 1984. Participation of diotoms in the amino-acid cycle of coastal waters uptake and excretion in cultures. Marine Ecology - Prowess Sf-ries. I ~(:1I. :lO:1-306. Ahmed, 8.T.; King, 8. L., and Clayton, J.R., 1984. Organic-mattler diagenesis in the anoxic sediments of Saanich Inlet. British Columbia. Canada - a case for highly evolved community interactions. Marine Chemistry. 14(3),233-252 Ajebouri, M.M. and Trollope, D.H., 1984. Indicator hacte'ia in fresh water and marine moUusks. HydrobioloRY, 111 (2), 9:l-1 02. Alam, M.; Piper, D.J.W., and Cooke, H.B.8., 198:\. Late Quaternarv stratigraphy and paleooceanography of the Crand Banks continental margin, eastern Canada. Boreas. \2(41. 25:1-2GI AIdabas, M.A.; Hybbard, F.H. , and McManus, J., 1984. The shell of Mytilus as an indicator of zonal variations of water quality within an estuary. Estuarine. Coastal and SI"'lf Science. I H(:ll. 2G:I-270. Allen, D.M., 1984. Population dynamics of the mysid shrimp Mysidop.,i., bili,-loll'i Tattersall. W.M. in a tern perate estuary. Jour nal of Crustacean Biology_ 4( 1).25':14 Allen, L.G. and Demartin, E.E., 198:\. Temporal and spatial patterns of nearshore distribution and abundance of the pelagic fishes off San Onofre Oceanside. Califol1lia. Fishery Rulll·tin, RI(:11. -
1 We Thank the Referees for Their Careful Review
We thank the referees for their careful review and thoughtful comments. Below please see our point-by-point responses and changes made to the manuscript. Referee report #1 Thank you for responding to my comments. It is now clearer what is going on, but some additional enhancements are desirable. You need to state clearly in the abstract and probably in the manuscript as well that you are using pre-industrial conditions to examine sea-ice generated Antarctic precipitation variability in the absence of anthropogenic forcing. This should appear explicitly in the first sentence of the abstract, I think, rather than being implicit here and throughout the manuscript. I am recommending minor revisions, but think that this is a very important aspect to address comprehensively to make the intent and methodology of your extensive work obvious to the reader. Done as suggested. Now the first sentence of the abstract reads “We conduct sensitivity experiments using a general circulation model that has an explicit water source tagging capability forced by prescribed composites of pre-industrial sea ice concentrations (SIC) and corresponding sea surface temperatures (SST) to understand the impact of sea ice anomalies on regional evaporation, moisture transport, and source–receptor relationships for Antarctic precipitation in the absence of anthropogenic forcing.” A similar statement is also made in the summary paragraph of the Introduction section: “In this study, we aim to understand the impact of SO sea ice anomalies associated with internal variability (in the absence of anthropogenic forcing) on local evaporation, moisture transport and source–receptor relationships for moisture and precipitation over Antarctica using a GCM that has an explicit water source tagging capability.” Section 3.2: You attribute southerly katabatic flow to the polar high. -
56. Otariidae and Phocidae
FAUNA of AUSTRALIA 56. OTARIIDAE AND PHOCIDAE JUDITH E. KING 1 Australian Sea-lion–Neophoca cinerea [G. Ross] Southern Elephant Seal–Mirounga leonina [G. Ross] Ross Seal, with pup–Ommatophoca rossii [J. Libke] Australian Sea-lion–Neophoca cinerea [G. Ross] Weddell Seal–Leptonychotes weddellii [P. Shaughnessy] New Zealand Fur-seal–Arctocephalus forsteri [G. Ross] Crab-eater Seal–Lobodon carcinophagus [P. Shaughnessy] 56. OTARIIDAE AND PHOCIDAE DEFINITION AND GENERAL DESCRIPTION Pinnipeds are aquatic carnivores. They differ from other mammals in their streamlined shape, reduction of pinnae and adaptation of both fore and hind feet to form flippers. In the skull, the orbits are enlarged, the lacrimal bones are absent or indistinct and there are never more than three upper and two lower incisors. The cheek teeth are nearly homodont and some conditions of the ear that are very distinctive (Repenning 1972). Both superfamilies of pinnipeds, Phocoidea and Otarioidea, are represented in Australian waters by a number of species (Table 56.1). The various superfamilies and families may be distinguished by important and/or easily observed characters (Table 56.2). King (1983b) provided more detailed lists and references. These and other differences between the above two groups are not regarded as being of great significance, especially as an undoubted fur seal (Australian Fur-seal Arctocephalus pusillus) is as big as some of the sea lions and has some characters of the skull, teeth and behaviour which are rather more like sea lions (Repenning, Peterson & Hubbs 1971; Warneke & Shaughnessy 1985). The Phocoidea includes the single Family Phocidae – the ‘true seals’, distinguished from the Otariidae by the absence of a pinna and by the position of the hind flippers (Fig. -
Data Structure
Data structure – Water The aim of this document is to provide a short and clear description of parameters (data items) that are to be reported in the data collection forms of the Global Monitoring Plan (GMP) data collection campaigns 2013–2014. The data itself should be reported by means of MS Excel sheets as suggested in the document UNEP/POPS/COP.6/INF/31, chapter 2.3, p. 22. Aggregated data can also be reported via on-line forms available in the GMP data warehouse (GMP DWH). Structure of the database and associated code lists are based on following documents, recommendations and expert opinions as adopted by the Stockholm Convention COP6 in 2013: · Guidance on the Global Monitoring Plan for Persistent Organic Pollutants UNEP/POPS/COP.6/INF/31 (version January 2013) · Conclusions of the Meeting of the Global Coordination Group and Regional Organization Groups for the Global Monitoring Plan for POPs, held in Geneva, 10–12 October 2012 · Conclusions of the Meeting of the expert group on data handling under the global monitoring plan for persistent organic pollutants, held in Brno, Czech Republic, 13-15 June 2012 The individual reported data component is inserted as: · free text or number (e.g. Site name, Monitoring programme, Value) · a defined item selected from a particular code list (e.g., Country, Chemical – group, Sampling). All code lists (i.e., allowed values for individual parameters) are enclosed in this document, either in a particular section (e.g., Region, Method) or listed separately in the annexes below (Country, Chemical – group, Parameter) for your reference. -
Brucella Antibody Seroprevalence in Antarctic Seals (Arctocephalus Gazella, Leptonychotes Weddellii and Mirounga Leonina)
Vol. 105: 175–181, 2013 DISEASES OF AQUATIC ORGANISMS Published September 3 doi: 10.3354/dao02633 Dis Aquat Org Brucella antibody seroprevalence in Antarctic seals (Arctocephalus gazella, Leptonychotes weddellii and Mirounga leonina) Silje-Kristin Jensen1,2,*, Ingebjørg Helena Nymo1, Jaume Forcada3, Ailsa Hall2, Jacques Godfroid1 1Section for Arctic Veterinary Medicine, Norwegian School of Veterinary Science, Stakkevollveien 23, 9010 Tromsø, Norway; member of the Fram Centre - High North Research Centre for Climate and the Environment, 9296 Tromsø, Norway 2Sea Mammal Research Unit, Scottish Oceans Institute, University of St. Andrews, St. Andrews KY16 8LB, UK 3British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK ABSTRACT: Brucellosis is a worldwide infectious zoonotic disease caused by Gram-negative bac- teria of the genus Brucella, and Brucella infections in marine mammals were first reported in 1994. A serosurvey investigating the presence of anti-Brucella antibodies in 3 Antarctic pinniped spe- cies was undertaken with a protein A/G indirect enzyme-linked immunosorbent assay (iELISA) and the Rose Bengal test (RBT). Serum samples from 33 Weddell seals Leptonychotes weddelli were analysed, and antibodies were detected in 8 individuals (24.2%) with the iELISA and in 21 (65.6%) with the RBT. We tested 48 southern elephant seal Mirounga leonina sera and detected antibodies in 2 animals (4.7%) with both the iELISA and the RBT. None of the 21 Antarctic fur seals Arctocephalus gazella was found positive. This is the first report of anti-Brucella antibodies in southern elephant seals. The potential impact of Brucella infection in pinnipeds in Antarctica is not known, but Brucella spp. -
Validation of Reanalysis Southern Ocean Atmosphere Trends Using Sea Ice Data
Atmos. Chem. Phys., 20, 14757–14768, 2020 https://doi.org/10.5194/acp-20-14757-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Validation of reanalysis Southern Ocean atmosphere trends using sea ice data William R. Hobbs1,3,5, Andrew R. Klekociuk2,3, and Yuhang Pan4 1Institute for Marine and Antarctic Studies (IMAS), University of Tasmania, Hobart, TAS 7001, Australia 2Antarctica and the Global System Program, Australian Antarctic Division, 203 Channel Highway, Kingston, TAS 7050, Australia 3Australian Antarctic Program Partnership, IMAS, University of Tasmania, Hobart, TAS 7001, Australia 4School of Earth Sciences, McCoy Building, The University of Melbourne, Parkville, VIC 3010, Australia 5ARC Centre of Excellence for Climate Extremes, IMAS, University of Tasmania, Hobart, TAS 7001, Australia Correspondence: William R. Hobbs ([email protected]) Received: 11 June 2020 – Discussion started: 29 July 2020 Revised: 5 October 2020 – Accepted: 23 October 2020 – Published: 2 December 2020 Abstract. Reanalysis products are an invaluable tool for rep- ing of West Antarctic ice shelves (Lenaerts et al., 2017; Paolo resenting variability and long-term trends in regions with et al., 2018; Dotto et al., 2019), with implications for global limited in situ data, and especially the Antarctic. A compar- barystatic sea level rise (Dupont and Alley, 2005; Pritchard ison of eight different reanalysis products shows large dif- et al., 2012; Paolo et al., 2015), and polar winds are clearly ferences in sea level pressure and surface air temperature related to observed Antarctic sea ice trends (Holland and trends over the high-latitude Southern Ocean, with implica- Kwok, 2012). -
2019 Weddell Sea Expedition
Initial Environmental Evaluation SA Agulhas II in sea ice. Image: Johan Viljoen 1 Submitted to the Polar Regions Department, Foreign and Commonwealth Office, as part of an application for a permit / approval under the UK Antarctic Act 1994. Submitted by: Mr. Oliver Plunket Director Maritime Archaeology Consultants Switzerland AG c/o: Maritime Archaeology Consultants Switzerland AG Baarerstrasse 8, Zug, 6300, Switzerland Final version submitted: September 2018 IEE Prepared by: Dr. Neil Gilbert Director Constantia Consulting Ltd. Christchurch New Zealand 2 Table of contents Table of contents ________________________________________________________________ 3 List of Figures ___________________________________________________________________ 6 List of Tables ___________________________________________________________________ 8 Non-Technical Summary __________________________________________________________ 9 1. Introduction _________________________________________________________________ 18 2. Environmental Impact Assessment Process ________________________________________ 20 2.1 International Requirements ________________________________________________________ 20 2.2 National Requirements ____________________________________________________________ 21 2.3 Applicable ATCM Measures and Resolutions __________________________________________ 22 2.3.1 Non-governmental activities and general operations in Antarctica _______________________________ 22 2.3.2 Scientific research in Antarctica __________________________________________________________ -
Observations on Penguins in the King Haakon VII Sea, Antarctica P.R
S. Afr. J. Antarct. Res., Vol. 9, 1979 29 Observations on penguins in the King Haakon VII Sea, Antarctica P.R. Condy Mammal Research Institute, University of Pretoria, Pretoria 0002 Data 011 penguin density, species composition, group size and and the surface nature of a floe was recorded as being either distribution were collected during the course of a seal census in smooth or hummocked. lee floes which were only partly pack ice in the King Haakon VII Sea, Antarctica, in January hummocked presented difficulties when classifying surface and February 1977. A total of 774 Addie mu/ 39 emperor pen structure, and only that part of the floe which was occupied guins were counted witl1in the 0,4 km wide cens1ts strips. An was classified. Penguins tended to move about a floe if the area of 288,17 km'!. of pack ice was censused and Adr'!lie and ship passed close by, so only the surface nature of that part emperor penguins occurred at densities of 2,69 and 0,14 indi of the floc occupied by them when they were first SCCil was viduals per km2 respecth·dy. Mean group size was 3,72 +3,76 classified. (n~J83) and 1,17±0,38 (n--~29) respecth·ely. Mean pack ice Observations were made from the ship's bridge 10 m above conce1/lration throughout the census was 0,48 ±0,25 tenths the waterline, and the limits of the 200 m census strips on (n~336). Both species were sem in all ice conditions, being either side of the ship were estimated using a sighting board more numerous in open to medium ice concentrations. -
A Specially Protected Species Under Annex II
WP 27 Agenda Item: CEP 8(b) Presented by: SCAR Original: English Current Status of the Ross Seal (Ommatophoca rossii): A Specially Protected Species under Annex II Attachments: atcm30_att030_e.pdf: Summary of status of the Ross seal. 1 WP 27 Current Status of the Ross Seal (Ommatophoca rossii): A Specially Protected Species under Annex II Introduction 1. Resolution 2 (1999) of XXIII ATCM requested SCAR, in consultation with the Parties, CCAMLR and other expert bodies as appropriate, to examine the status of the species currently designated in Appendix A of Annex II to the Environmental Protocol, and with the assistance of IUCN, to determine the conservation status of native Antarctic fauna and flora and advise the CEP on which species should remain or be designated as Specially Protected Species. 2. At XXIII ATCM an Intersessional Contact Group, chaired by Argentina, was established to discuss the criteria that could be used to designate Specially Protected Species. The Final ICG report was presented as XXV ATCM/ WP8. The advice to the ATCM was encapsulated in Resolution 1 (2002), which noted that the CEP had decided to adopt the IUCN criteria on endangerment to establish the degree of threat to species, requested SCAR to assist in reviewing those species which were classed as “vulnerable”, “endangered” or “critically endangered” (taking into consideration regional assessments of populations), as well as reviewing those species classed as “data deficient” or “near threatened” which occurred in the Antarctic Treaty Area. 3. Working Paper XXVIII ATCM WP34 proposed how the IUCN criteria could be applied to Antarctic species. At XXIX ATCM SCAR tabled WP39 proposing that, on this basis and on the grounds of the presently available population data, Antarctic Fur Seals (Arctocephalus spp.) should be delisted as Specially Protected Species. -
The Antarctic Ross Seal, and Convergences with Other Mammals
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Servicio de Difusión de la Creación Intelectual Evolutionary biology Sensory anatomy of the most aquatic of rsbl.royalsocietypublishing.org carnivorans: the Antarctic Ross seal, and convergences with other mammals Research Cleopatra Mara Loza1, Ashley E. Latimer2,†, Marcelo R. Sa´nchez-Villagra2 and Alfredo A. Carlini1 Cite this article: Loza CM, Latimer AE, 1 Sa´nchez-Villagra MR, Carlini AA. 2017 Sensory Divisio´n Paleontologı´a de Vertebrados, Museo de La Plata, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, La Plata, Argentina. CONICET, La Plata, Argentina anatomy of the most aquatic of carnivorans: 2Pala¨ontologisches Institut und Museum der Universita¨tZu¨rich, Karl-Schmid Strasse 4, 8006 Zu¨rich, Switzerland the Antarctic Ross seal, and convergences with MRS-V, 0000-0001-7587-3648 other mammals. Biol. Lett. 13: 20170489. http://dx.doi.org/10.1098/rsbl.2017.0489 Transitions to and from aquatic life involve transformations in sensory sys- tems. The Ross seal, Ommatophoca rossii, offers the chance to investigate the cranio-sensory anatomy in the most aquatic of all seals. The use of non-invasive computed tomography on specimens of this rare animal Received: 1 August 2017 reveals, relative to other species of phocids, a reduction in the diameters Accepted: 12 September 2017 of the semicircular canals and the parafloccular volume. These features are independent of size effects. These transformations parallel those recorded in cetaceans, but these do not extend to other morphological features such as the reduction in eye muscles and the length of the neck, emphasizing the independence of some traits in convergent evolution to aquatic life. -
1 Influence of Sea Ice Anomalies on Antarctic Precipitation Using
https://doi.org/10.5194/tc-2019-69 Preprint. Discussion started: 12 June 2019 c Author(s) 2019. CC BY 4.0 License. Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution Hailong Wang1*, Jeremy Fyke2,3, Jan Lenaerts4, Jesse Nusbaumer5,6, Hansi Singh1, David Noone7, and Philip Rasch1 (1) Pacific Northwest National Laboratory, Richland, WA 5 (2) Los Alamos National Laboratory, Los Alamos, NM (3) Associated Engineering, Vernon, British Columbia, Canada (4) Department of Atmospheric and Oceanic Sciences, University of Colorado at Boulder, Boulder, CO (5) NASA Goddard Institute for Space Studies, New York, NY (6) Center for Climate Systems Research, Columbia University, New York, NY 10 (7) Oregon State University, Corvallis, OR *Correspondence to: [email protected] 1 https://doi.org/10.5194/tc-2019-69 Preprint. Discussion started: 12 June 2019 c Author(s) 2019. CC BY 4.0 License. Abstract We conduct sensitivity experiments using a climate model that has an explicit water source tagging capability forced by prescribed composites of sea ice concentrations (SIC) and corresponding SSTs to understand the impact of sea ice anomalies on regional evaporation, moisture transport, and source– 5 receptor relationships for precipitation over Antarctica. Surface sensible heat fluxes, evaporation, and column-integrated water vapor are larger over Southern Ocean (SO) areas with lower SIC, but changes in Antarctic precipitation and its source attribution with SICs reflect a strong spatial variability. Among the tagged source regions, the Southern Ocean (south of 50°S) contributes the most (40%) to the Antarctic total precipitation, followed by more northerly ocean basins, most notably the S. -
UNIVERSITY of CALIFORNIA, MERCED Contribution of Sources
UNIVERSITY OF CALIFORNIA, MERCED Contribution of sources and sinks to the photochemistry of the present and past atmosphere of West Antarctica based on air, snow and ice-core records A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Environmental Systems by Sylvain Masclin Committee in charge: Professor Wolfgang F. Rogge, Chair Professor Roger C. Bales Professor Martha H. Conklin Dr. Markus M. Frey 2014 Copyright Sylvain Masclin, 2014 All rights reserved. The dissertation of Sylvain Masclin is approved, and it is acceptable in quality and form for publication on microfilm and electronically: Roger C. Bales, Advisor Martha H. Conklin Markus M. Frey, Co-Advisor Wolfgang F. Rogge, Chair University of California, Merced 2014 iii ABSTRACT A framework is presented for defining the present atmospheric chemistry of West Antarctica and the photochemistry of the atmosphere during the early- to mid-Holocene transition (9,000-6,000 yr BP). Little is known on the contributions of local and regional sources to the photochemical composition of the current atmosphere of West Antarctica and the early- to mid-Holocene atmosphere. Measurements over the West Antarctic continent were scarce in regards of exploring its present photochemical composition, while the contribution of the atmospheric oxidative capacity, namely OH radicals, to the methane decline over the early- to mid-Holocene has been assumed negligible. In this study, investigation of the present atmospheric chemistry was run during Antarctic summer at the WAIS Divide site, through multi-week continuous measurements of - - photochemical active species: atmospheric NO, O3, H2O2, MHP, and snow NO3 , NO2 and H2O2.