Journal articles: 'East of Bay'

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Katherine Vaz. "East Bay Grease." Antioch Review 74-75, no. 4-1 (2017): 1030. http://dx.doi.org/10.7723/antiochreview.74-75.4-1.1030.

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Vaz, Katherine. "East Bay Grease." Antioch Review 62, no. 3 (2004): 416. http://dx.doi.org/10.2307/4614681.

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Abraham, Kenneth F., Christopher M. Sharp, and Peter M. Kotanen. "Habitat change at a multi-species goose breeding area on Southampton Island, Nunavut, Canada, 1979–2010." Arctic Science 6, no. 2 (June 1, 2020): 95–113. http://dx.doi.org/10.1139/as-2018-0032.

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Foraging by hyperabundant Arctic-nesting geese has significant impacts on vegetation of Arctic and subarctic coastal lowlands, but long-term data sets documenting these changes are rare. We undertook intensive surveys of plant communities at East Bay and South Bay, Southampton Island, Nunavut, Canada, in July 2010. Lesser Snow Geese, Ross’s Geese, Cackling Geese, and Brant nest and rear young at these sites; the first three have experienced up to 10-fold increases since the 1970s. At East Bay, we found significant declines in graminoids over the 31-year span, as well as significant declines in lichen and willow cover, and significant increases in rock cover. Transect data indicated graminoids were present at only 15%–36% of points at East Bay, whereas at South Bay, graminoids were present at 28%–90% of points. Moss was more prominent in transects at South Bay than at East Bay (40%–85% vs. 19%–42%), but quadrat data indicated much more of the moss cover at South Bay apparently was dead than at East Bay. Puccinellia phryganodes (Trin.) Scribn. & Merr. exceeded 1% in only two transects. Our data demonstrate a striking decline of preferred forage species and increases in non-forage cover, consistent with the hypothesis that changes resulted from persistent long-term foraging by the four species of breeding geese between spring arrival and late summer departure.

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Wang, Ruifu, Pan Wei, and Yingjie Zhao. "Analysis of Influence Factors of GF-4 Registration Accuracy on Sea Ice Drift in the Bohai Sea." E3S Web of Conferences 131 (2019): 01073. http://dx.doi.org/10.1051/e3sconf/201913101073.

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The “GF-4” satellite is China’s first high resolution geostationary optical remote sensing satellite. It has the unique advantages of short imaging time interval (20s) and high resolution (50m). In order to analyze the effect of GF-4 satellite image registration accuracy on sea ice drift in Bohai Sea, firstly, the orthorectification of the 28 image data available from August 2016 to March 2018 in the Bohai Sea area was carried out. Then we selected the sea-land edge points as control points, and registration of two images which have the same time interval. Next, we recorded the marked same name points which searched from the bottom of Liaodong bay, east of Liaodong bay and west of Liaodong bay respectlly. We statisticed the direction and frequency of land point offset sub-regionally, then we created the rose plots and maked histogram of the offset of land point. The results show that, when the time interval is 4 hours and 24 hours, the dominant migration direction in the three regions in Liaodong bay is east; when the time interval is 1 minute, the dominant migration direction in Liaodong Bay bottom and Liaodong Bay west coast land is south, Followed by east and southeast respectively; the dominant migration in Liaodong Bay East Coast is north, followed by east; When the time interval is 3 hours, the dominant migration direction in west of Liaodong Bay, bottom of Liaodong Bay and east of Liaodong bay are east, west and south respectively, followed by southeast, east, southeast respectively. The land offset in three regions is major centralized distribution in a range which is from 60m to 80m. That is to say, the offset of land is basically equal to 1.2 times of pixels, and the maximum land offset is less than 2 times of pixels. Through statistical analysis, it can be seen that with the increase of time interval, the land offset will not change much. This study also paves the way for the study of the drift of sea ice.

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Glickenstein, Harvey. "Bay Area Rapid Transit Extension South on the East Bay [Transportation Systems]." IEEE Vehicular Technology Magazine 12, no. 3 (September 2017): 12–16. http://dx.doi.org/10.1109/mvt.2017.2717323.

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Perkins, Deborah E., Paul A. Smith, and H. Grant Gilchrist. "The breeding ecology of ruddy turnstones (Arenaria interpres) in the eastern Canadian Arctic." Polar Record 43, no. 2 (March 28, 2007): 135–42. http://dx.doi.org/10.1017/s0032247407006092.

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In 2002 and 2003, studies were made of the breeding phenology, nesting success, nesting density, and rates of nest predation of ruddy turnstones (Arenaria interpres) at East Bay, Southampton Island, Nunavut, Canada. Previous data from East Bay were used to compare nesting chronology and nest success across years. Bird banding data were used to examine migration routes and rates of return. In all years, ruddy turnstones initiated nests within 7 days of arrival at the study area. The median date of incubation onset was the same in 2002 and 2003, despite different spring snow conditions. Snow remained later in the season in 2003 and the overall range of incubation onset was greater than in 2002. Ruddy turnstones at East Bay nested at high densities and in semi-colonial groups with a significantly aggregated distribution. In both years, nest success was low, predation was high, and lemmings were scarce. These data (and data from earlier East Bay studies) support the ‘alternative prey hypothesis’. Resighting rates of breeding adults between 2002 and 2003 were also low. Individuals banded at East Bay were resighted at Delaware Bay on the Atlantic coast of the United States, the Caribbean Islands, and in southern Brazil. This study increases our knowledge of this understudied species about which there is conservation concern.

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Norman, F. I. "The East German East Antarctic Expedition, 1979–80." Polar Record 40, no. 3 (July 2004): 253–60. http://dx.doi.org/10.1017/s003224740400364x.

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A once-restricted report dealing with the first (and only) official East German Antarctic expedition to Prydz Bay, East Antarctica, is discussed. Members of ‘die Ergebnisse der DDR-Erkundungsexpedition’ (EREX 79/80) were in the Larsemann Hills during the 1979–80 season. From ground (17 January) and aerial examination (17 January, 8 February), a site on eastern Broknes was selected for a future station; proposed facilities and some EREX observations are presented. Implications and consequences of the visit are discussed in relation to subsequent station development in the Larsemann Hills.

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Yang, Huayun, Bin Xue, Lixia Jin, Shanshan Zhou, and Weiping Liu. "Polychlorinated biphenyls in surface sediments of Yueqing Bay, Xiangshan Bay, and Sanmen Bay in East China Sea." Chemosphere 83, no. 2 (March 2011): 137–43. http://dx.doi.org/10.1016/j.chemosphere.2010.12.070.

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Mehmood, Tariq, Syed Waseem Haider, and Saima Siddiqui. "Major, Minor and Trace Elements Existence in Surface Sediments from Gwadar to Jiwani Coastal Areas of Pakistan." International Journal of Economic and Environmental Geology 11, no. 2 (September 25, 2020): 37–45. http://dx.doi.org/10.46660/ijeeg.vol11.iss2.2020.444.

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This study was carried out along the western coastal parts of Balochistan from Gwadar east Bay to Jiwani. The local anomaly of major, minor and trace elements were studied in this area. Zone-I (Gwadar east and west Bay) indicates that calcium oxide, potassium oxide and titanium dioxide have higher or average concentrations, while ZoneII indicates higher or average concentrations of calcium oxide, titanium dioxide and ferric oxide. Trace elements zirconium, chromium, europium, strontium, and copper are in higher or average concentrations in both zones. Gwadar west Bay and Jiwani are intermediate in carbonate, which show a high degree of maturity, suggesting the high rate of weathering in the source area. Sediment samples from Ganz, Jiwani, and Gwadar east Bay represent the quartz-rich fields in this region. Gwadar east Bay has a positive correlation between aluminium oxide and potassium oxide which suggests that abundance of potassium oxide is controlled by variation in K-feldspar contents. A positive correlation between strontium and calcium oxide suggests that strontium is associated with calcium oxide in biogenic carbonate material in Gwadar west Bay. The positive correlation between aluminium oxide, copper, and zinc in Pishukan indicates that the abundance of these elements is due to limited silt and clay fractions present in sediments. Enrichment factor shows that chromium and strontium are probably of anthropogenic origin in this region. Keywords

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Sønderholm, M., and H. Tirsgaard. "Lithostratigraphic framework of the Upper Proterozoic Eleonore Bay Supergroup of East and North-East Greenland." Bulletin Grønlands Geologiske Undersøgelse 167 (January 1, 1993): 1–38. http://dx.doi.org/10.34194/bullggu.v167.6723.

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In the region between Canning Land (71° 30’N) and Bessel Fjord (76°N) the Eleonore Bay Supergroup is up to 16 km thick and comprises both metasediments and sediments. It is divided into five new groups. In the eastern outcrops four groups are found; these are from base to top: the Nathorst Land Group (up to c. II 000 m thick), the Lyell Land Group (2000-2800 m thick), the Ymer Ø Group (900-1300 m thick) and the Andrée Land Group (900-1500 m thick). The lower two of these groups consist of altemating sandstones and mudstones (and their metamorphic equivalents). Information on the depositional environment of the Nathorst Land Group is scarce, but both fluvial and marine settings have been tentatively proposed. The Lyell Land Group mainly represents marine shelf environments. The Ymer Ø and Andrée Land Groups are dominated by carbonates deposited in a platform, slope and basinal environment. Furthest west, in the nunatak region, a succession of sandstones and mudstones more than 6300 m thick is included in the Petermann Bjerg Group. The stratigraphic relationship between the Petermann Bjerg Group and the rest of the Eleonore Bay Supergroup is uncertain but possibly correlates with parts of the Nathorst Land and Lyell Land Groups. The Eleonore Bay Supergroup is finally compared with other Upper Proterozoic successions in the North Atlantic region.

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Cerrano, Carlo, Giorgio Bavestrello, Barbara Calcinai, Riccardo Cattaneo-Vietti, and Antonio Sarà. "Asteroids eating sponges from Tethys Bay, East Antarctica." Antarctic Science 12, no. 4 (December 2000): 425–26. http://dx.doi.org/10.1017/s095410200000050x.

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In many Antarctic benthic communities, sponges can be considered as keystone species on both hard and soft bottoms, affecting community structure and sediment texture (Cattaneo-Vietti et al. 2000). Moreover, Antarctic sponges are known to be exploited by numerous organisms as atrophic source. The most important Antarctic sponge predators are asteroids and molluscs which move and digest slowly. The activity of invertebrate predators is not affected by the sponge nutritional composition: toxicity and relative abundance are considered to be the most important factors regulating predation on the Antarctic sponge fauna (McClintock 1987).

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Barbara, Loïc, Xavier Crosta, Guillaume Massé, and Olivier Ther. "Deglacial environments in eastern Prydz Bay, East Antarctica." Quaternary Science Reviews 29, no. 19-20 (September 2010): 2731–40. http://dx.doi.org/10.1016/j.quascirev.2010.06.027.

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Pello, F. S., and R. Pentury. "Phytoplankton of Inner Ambon bay during east monsoon." IOP Conference Series: Earth and Environmental Science 517 (June 20, 2020): 012003. http://dx.doi.org/10.1088/1755-1315/517/1/012003.

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Quach, Tommy, Luis Colon, Akintayo Akinrinlola, Jesse Bell, and Sonya Good. "Assessing the East Bay of Galveston Bay, Texas for Coliform Bacteria in Recreational Water." Open Journal of Marine Science 06, no. 04 (2016): 472–81. http://dx.doi.org/10.4236/ojms.2016.64039.

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15

Gabsatarova, Irina, B. Assinovskaya, S. Baranov, V. Karpinsky, D. Mehryushev, L. Munirova, L. Nadezhka, S. Petrov, S. Pivovarov, and I. Sanina. "EAST EUROPEAN PLATFORM. RUSSIAN PART." Earthquakes in Northern Eurasia, no. 23 (December 15, 2020): 199–207. http://dx.doi.org/10.35540/1818-6254.2020.23.19.

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It is reported that 22 stationary seismic stations, 2 arrays and 7 local seismic stations, located in the area of Novovoronezh and Kursk nuclear stations, monitor seismicity of the Russian territory of the East European platform (EEP). A new station Belogornoe with high registration class has been opened, which also belongs to the International Monitoring System for the Comprehensive Nuclear-Test-Ban Treaty (IMS CTBTO). The results of the microseismic noise study at the Pulkovo network stations and assessment of maximum distance of earthquake registration in the Voronezh crystalline massif are presented. In 2014, relatively strong earthquakes with М3.0 were not recorded on the Russian territory of the EEP. Weaker natural seismicity with M≤2 was recorded in Karelia and the border areas with Finland, near Kandalaksha Bay, near the Khibiny Massif on the Kola Peninsula and on the territory of the Voronezh Crystalline Massif. Observations of local networks near nuclear stations are aimed at updating the information on seismicity previously considered as an aseismic territory of the EEP. Man-made events were recorded in permanent quarries, the most powerful of them (M=3.1–3.3) were produced in the quarries on the territory of the Kursk magnetic anomaly.

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Zhang, Chun Hua, Xiao Qing Han, Jing Li, Wei Zhang, Kai Wu, and Wei Ming Gao. "The Study of Environmental Characteristic by Coastal Engineering in Rock Coast." Applied Mechanics and Materials 226-228 (November 2012): 1308–11. http://dx.doi.org/10.4028/www.scientific.net/amm.226-228.1308.

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In order to study the evolvement of rock coastal in Hebei Province, the data was taken to study the evolved stations, such as relief maps, charts, remote sensing imagines and the field data of different areas from 1956 to 2007. With 3 S technology, it analyzed the evolvement processing and reasons of the rock coast by construction of coastal engineering in half century. The results were shown that it was changed strongly by the station from 1979 to 2007 when the station stopped the littoral current caused by coastal engineering such as Qinhuandgao Port and Shanhaiguan Shipyard. As the result, the section was deposited in the east of Qinhuangdao Port while eroded in the west. And the highest erosion speed was 2.49 m/a in the section from Xinkaihe River to South Mountain shipside. The angle was about 60°~80° from between middle bay and east bay. By the transport yield reduce of Tanghe River and Chituhe River, the coastline was eroded by NNE and ENE waves. Without the supply of sediment from the east bay and middle bay where were eroded seriously, the erosion speed was above 3.26 m/a, and the section was eroded fast with the speed of 3.67 m/a between Jinshan Mountain and Tiger Stone in west bay.

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Woehler, EJ, B. Raymond, and DJ Watts. "Decadal-scale seabird assemblages in Prydz Bay, East Antarctica." Marine Ecology Progress Series 251 (2003): 299–310. http://dx.doi.org/10.3354/meps251299.

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Yang, Dongfang, Junhui Guo, Yinjiang Zhang, Ziru Ding, and Zhiguo Bu. "Pb Distribution and Sources in Jiaozhou Bay, East China." Journal of Water Resource and Protection 03, no. 01 (2011): 41–49. http://dx.doi.org/10.4236/jwarp.2011.31005.

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Shibuya, K., Y. Fukuda, and Y. Michida. "Determination of geoid height at Breid Bay, east Antarctica." Journal of Geophysical Research 96, B11 (1991): 18285. http://dx.doi.org/10.1029/91jb01810.

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Matsubara, S., and Y. Motoyosh. "Potassium pargasite from Einstödingen, Lützow-Holm Bay, East Antarctica." Mineralogical Magazine 49, no. 354 (December 1985): 703–7. http://dx.doi.org/10.1180/minmag.1985.049.354.09.

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AbstractPotassium pargasite containing 3.19 wt. % K2O was found in a skarn from the islet of Einstödingen, Lützow-Holm Bay, East Antarctica, together with some high potassium pargasitic amphiboles. A positive correlation is shown between Fe2+/(Mg+Fe2+) and K/(K + Na(A)) ratios in pargasitic amphiboles suggesting that the increase of Fe2+ serve to stabilize high-K pargasites under the metamorphic conditions of the granulite facies.

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Gräwe, U., J. O. Wolff, and J. Ribbe. "Impact of climate variability on an east Australian bay." Estuarine, Coastal and Shelf Science 86, no. 2 (January 2010): 247–57. http://dx.doi.org/10.1016/j.ecss.2009.11.020.

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Kusahara, Kazuya, Daisuke Hirano, Masakazu Fujii, Alexander D. Fraser, and Takeshi Tamura. "Modeling intensive ocean–cryosphere interactions in Lützow-Holm Bay, East Antarctica." Cryosphere 15, no. 4 (April 7, 2021): 1697–717. http://dx.doi.org/10.5194/tc-15-1697-2021.

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Abstract. Basal melting of Antarctic ice shelves accounts for more than half of the mass loss from the Antarctic ice sheet. Many studies have focused on active basal melting at ice shelves in the Amundsen–Bellingshausen seas and the Totten ice shelf, East Antarctica. In these regions, the intrusion of Circumpolar Deep Water (CDW) onto the continental shelf is a key component for the localized intensive basal melting. Both regions have a common oceanographic feature: southward deflection of the Antarctic Circumpolar Current brings CDW toward the continental shelves. The physical setting of the Shirase Glacier tongue (SGT) in Lützow-Holm Bay corresponds to a similar configuration on the southeastern side of the Weddell Gyre in the Atlantic sector. Here, we conduct a 2–3 km resolution simulation of an ocean–sea ice–ice shelf model using a recently compiled bottom-topography dataset in the bay. The model can reproduce the observed CDW intrusion along the deep trough. The modeled SGT basal melting reaches a peak in summer and a minimum in autumn and winter, consistent with the wind-driven seasonality of the CDW thickness in the bay. The model results suggest the existence of an eastward-flowing undercurrent on the upper continental slope in summer, and the undercurrent contributes to the seasonal-to-interannual variability in the warm water intrusion into the bay. Furthermore, numerical experiments with and without fast-ice cover in the bay demonstrate that fast ice plays a role as an effective thermal insulator and reduces local sea ice formation, resulting in much warmer water intrusion into the SGT cavity.

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Pavlyuk, Olga N., and Julia A. Trebukhova. "Composition and distribution of meiobenthos in amursky bay (peter the great bay, the east sea)." Ocean Science Journal 40, no. 3 (September 2005): 10–16. http://dx.doi.org/10.1007/bf03022606.

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Wisha, Ulung Jantama, Try Al Tanto, and Ilham Ilham. "Physical and Chemical Conditions of Bayur Bay Waters On the East and West Season." ILMU KELAUTAN: Indonesian Journal of Marine Sciences 22, no. 1 (March 1, 2017): 15. http://dx.doi.org/10.14710/ik.ijms.22.1.15-24.

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Physical construction of Bayur bay coastal area as a port was followed by a variety of environmental issues, both physical degradation of the natural environment, biology reduction and an increase in social problems, directly affect to water quality decreasing in the coastal Bayur Bay. This study aims to determine the concentration distribution of physical and chemical parameters and their influence to water conditions on the east and west season. The method used is descriptive method (data taken by in situ and laboratory analysis), determining the location of sampling points based on purposive sampling method and tide prediction by NAOtide software. The results of field survey and laboratory measurements analysed using statistical method. The speed of sea currents on the east season ranged from 3,48 to 24,9 cm.s-1, while in the West season flow rate ranged from 1,4 to 57,7 cm.s-1. Rainfall in East Season ranged from 0-45 mm and The intensity of rainfall in West Season ranged from 0-30 mm. Sea-surface temperatures in the Eastern season range between 26,2- 31.5 °C, while in the west season SST range from 24,3 to 30,5°C. Dissolve oxygen concentration in the east season range from 4,3 to 6,1 mg.L-1, while the west monsoon conditions range from 4,1 to 6,4 mg.L-1. The pH values ranged from 7,4 to 8,1 in the Eastern season and ranged from 7,12 to 8,27 in the West season. Bayur Bay water quality conditions is not much different from its value range on the west and east season and influencing each other. Keywords: Bayur Bay, Seasons, SST, Statistical method

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Putri, Mutiara Rachmat, Iwan P. Anwar, Zetsaona Sihotang, Lamona I. Bernawis, Agus Setiawan, Muhammad Riza, Idris Mandang, and Willem M. Tatipatta. "Observation and numerical modeling of physical oceanography in the Balikpapan Bay, East Kalimantan: Preliminary results." Depik 10, no. 2 (June 23, 2021): 130–35. http://dx.doi.org/10.13170/depik.10.2.19259.

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The Indonesian government plans to move the capital city from Jakarta to Penajam Paser Utara (PPU) which is the upstream area of Balikpapan Bay, East Kalimantan. There are several activities in the planned new capital city that potentially affect the condition of land and marine ecosystems, including clearing new land for housing and agriculture as well as expanding mining and petroleum areas. Directly or indirectly, these activities could affect the oceanographic conditions of Balikpapan Bay. For this reason, in order to obtain an up-to-date picture of Balikpapan Bay, an oceanographic survey was conducted in early March 2020. In addition, to support the analysis of marine dynamics in these waters and their predictions in the future, numerical simulations of hydrodynamic modeling were also carried out. Oceanographic observations indicate significant water stratification in the area about 20 km from the mouth of the bay. This result is also well illustrated in the hydrodynamic model numerical simulation, where there is a water loop at the confluence between salt and fresh water masses from two rivers 18-20 km from the mouth of Balikpapan Bay. Keywords:The national capital city of IndonesiaBalikpapan BayPhysical oceanography ObservationCoastal and marine Ecosystem

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TANAKA, KATSUHIKO, YUKA YOKOYAMA, MIKIO FUJIMAKI, and IZUMI SAKAMOTO. "Macrobenthic fauna in Okirai Bay and Toni Bay, Iwate Prefecture, after the Great East Japan Earthquake." NIPPON SUISAN GAKKAISHI 84, no. 6 (November 15, 2018): 1050–53. http://dx.doi.org/10.2331/suisan.wa2567-2.

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Rowntree, Lester B. "Afforestation, Fire, and Vegetation Management in the East Bay Hills of the San Francisco Bay Area." Yearbook of the Association of Pacific Coast Geographers 56, no. 1 (1994): 7–30. http://dx.doi.org/10.1353/pcg.1994.0013.

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Warnock, Jonathan P., and Reed P. Scherer. "Increased diatom dissolution in Prydz Bay, East Antarctica linked to inception of the Prydz Bay gyre." Diatom Research 31, no. 2 (April 2, 2016): 161–68. http://dx.doi.org/10.1080/0269249x.2016.1182075.

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Francis, RICC, and RH Winstanley. "Differences in growth rates between habitats of South-east Australian snapper (Chrysophrys auratus)." Marine and Freshwater Research 40, no. 6 (1989): 703. http://dx.doi.org/10.1071/mf9890703.

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Data on recaptured fish from two tagging experiments on south-east Australian snapper, Chrysophrys auratus, were analysed: 198 fish released in several Victorian locations between 1956 and 1962, and 118 fish released in Port Phillip Bay in 1971 and 1972. Movement data from both experiments were used to classify the fish into habitats (oceanic and bay) and stocks (western and eastern). Length increment data from the earlier experiment indicate that the major growth-rate differences in south-east Australian snapper lie within the western stock (between oceanic and bay habitats) rather than between stocks as suggested by an earlier analysis of the same data. The annual growth rates of 20-30-cm snapper in Port Phillip Bay and Western Port are 17-20% higher than for fish in the ocean. Oceanic growth rates in the western stock appear to be lower than those in the eastern stock. Procedural differences in length measurements at tagging and recapture can introduce a net bias in the length increment that, if ignored (as is conventional in tagging growth models), will bias growth rate estimates. In the earlier tagging experiment, this is shown to have caused a 10% positive bias in growth rate estimates.

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Vutilolo, I. V. N., A. P. Tyagi, L. A. J. Thomson, and M. Heads. "Comparison of performance of whitewood (Endospermum medullosum L. S. Smith) provenances and families in Vanuatu." South Pacific Journal of Natural and Applied Sciences 23, no. 1 (2005): 37. http://dx.doi.org/10.1071/sp05007.

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This study reports a comparison of performance of four year-old whitewood (Endospermum medullosum L S Smith) provenances and families trials established by the Department of Forestry of Vanuatu and the South Pacific Regional Programme In Forest Genetic Resources project (SPRIG). Trees in the different open-pollinated, half-sibling families had mean heights ranging from 7.1 m to 10.2 m, dbh from 13.5 cm to 17.8 cm, wood volume from 0.07 to 0.14 m3 and survival from 54% to 91%. Seedlot GD11 from Shark Bay East Santo showed the superior mean height of 10.2 m followed by seedlot MT29 from Maewo and MS47 from Malel Central East Santo with 9.6 m. The shortest trees were in families JT35 (Forari, Efate) with 7.1 m, MT33 (Maewo) and JT30 (Forari, Efate) with 7.5 m. Trees in seedlots MS44 from Malel Central East Santo and MS32 from Palon East Santo had the biggest diameter increase(mean dbh of 17.8 cm) followed by seedlot GD11 Shark Bay East Santo and MS2 from Sara East Santo with 17.5 cm and MS55 from South East Santo with 17.4 cm. Seedlots with very low diameter increment were MT3 from Maewo and JT35 from Forari (mean dbh of 13.5 cm) followed by MT3 and MT4 from Central Pentecost with a mean dbh of 13.8 cm. Seedlots with superior wood volume production were MS2 from Sara East Santo (with mean of 0.15 m3 per tree) followed by seedlots MS32 Palon East Santo, GD11 Shark Bay East Santo, MS55 South East Santo with 0.14 m3 and MS3 Kole East Santo with 0.13 m3. The slowest growing seedlots were JT35 from Forari Efate and MT32 from Maewo with mean volume of 0.07 m3. Study reveals that there is a great potential among provenances and families for further improvement and to establish breeding programme to breed whitewood for higher quantity and better timber quality.

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Zhao, Y., X.-H. Liu, B. X.-C. Liu, Song L.-D. Liu, Y.-B. Wang, and P. Liu. "Pan-African Events in Prydz Bay, East Antarctica and its Inference on East Gondwana Tectonics." Gondwana Research 4, no. 4 (October 2001): 842–43. http://dx.doi.org/10.1016/s1342-937x(05)70624-9.

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Zhao, Y., X. H. Liu, X. C. Liu, and B. Song. "Pan-African events in Prydz Bay, East Antarctica, and their implications for East Gondwana tectonics." Geological Society, London, Special Publications 206, no. 1 (2003): 231–45. http://dx.doi.org/10.1144/gsl.sp.2003.206.01.12.

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Langdon, JS. "Haemosiderosis in Platycephalus bassensis and Diodon nicthemerus in south-east Australian coastal waters." Marine and Freshwater Research 37, no. 5 (1986): 587. http://dx.doi.org/10.1071/mf9860587.

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The degree of haemosiderin deposition in the spleen, liver, and kidney of P. bassensis and D. nicthemerus was compared in specimens from Port Phillip Bay, and Lakes Entrance, Victoria, Bass Strait, and the Derwent estuary, Tasmania. D. nicthemerus displayed extensive visceral haemosiderosis and fatty infiltration of the liver at all sites, apparently as normal conditions. P. bassensis from Port Phillip Bay displayed severe visceral haemosiderosis, whereas specimens from the remaining sites had only low background levels of haemosiderin deposition. It is suggested that high levels of visceral haemosiderin in fish species normally displaying low levels are indicative of a suboptimal health status in fish populations. No infectious cause of the haemosiderosis in Port Phillip Bay fish has been identified, and toxic or pollution-related causes are thus considered likely to be responsible.

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Weir, Caroline R., Jonathan Stokes, Clive Martin, and Pablo Cermeño. "Three sightings of Mesoplodon species in the Bay of Biscay: first confirmed True's beaked whales (M. mirus) for the north-east Atlantic?" Journal of the Marine Biological Association of the United Kingdom 84, no. 5 (October 2004): 1095–99. http://dx.doi.org/10.1017/s0025315404010525h.

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Three sightings of Mesoplodon beaked whales are reported from the Bay of Biscay, north-east Atlantic. All sightings comprised one or two animals, breaching repeatedly in proximity to the survey vessel, and occurred at between 2200 and 4100 m water depth. Descriptive and photographic data are compared with published accounts of Mesoplodon species in the north-east Atlantic, and the identification of the animals as True's beaked whale (Mesoplodon mirus) concurs with all observed features. Within the north-east Atlantic, True's beaked whale is the only Mesoplodon species that could produce the single, closely-spaced parallel-paired scar observed on one animal. Our observations are consistent with the first live sightings of True's beaked whale in the Bay of Biscay, and only the second documented record worldwide.

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Holloway, PE, G. Symonds, and Vaz R. Nunes. "Observations of circulation and exchange processes in Jervis Bay, New South Wales." Marine and Freshwater Research 43, no. 6 (1992): 1487. http://dx.doi.org/10.1071/mf9921487.

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This paper discusses oceanographic observations obtained in and near Jervis Bay, a small coastal embayment of approximately 124 km2 situated on the New South Wales coast, during a series of measurement programmes spanning three years. Various mechanisms that drive water circulation within the bay and water exchange between the bay and the adjacent continental shelf are discussed. Current meter data from within the bay show surprisingly little correlation with the wind. Currents are characterized by persistent flows in one direction for periods of months, and it is suggested that influences from the shelf are responsible for driving the bay circulation. Flow through the bay entrance is weakly correlated with the wind at a period of around eight days, with near-surface inflow on the southern side of the entrance being in phase with deeper outflow on the northern side and vice versa. The shelf waters are well known for their coastally trapped waves. These have the potential to oscillate vertically the density surfaces on the shelf on a time scale of around eight days, and observations indicate that these waves are an additional mechanism driving circulation in the bay. The shelf waters are influenced by the warm East Australia Current and its eddies, and this appears to maintain a density contrast between the bay and the shelf for most of the year, with the shelf waters being less dense, which may be an additional mechanism driving bay circulation. Current-meter data from the bay entrance show a persistent northward current component in contrast to the strong southward flow of the East Australia Current on the shelf. Conductivity-temperature- depth data reveal cold, dense water flowing out of the bay during periods of strong winter cooling and the effects of warm eddies pushing warm water into the bay and displacing cold deeper water away from the bay. The heating/cooling cycle of the bay appears to be influenced by advection processes on the shelf as well as by aidsea heat and radiation exchanges.

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36

de Graaf, Lawrence B., and Delores Nason McBroome. "Parallel Communities: African Americans in California's East Bay, 1850-1963." Journal of American History 81, no. 3 (December 1994): 1340. http://dx.doi.org/10.2307/2081558.

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37

Hui, Fengming, Tiancheng Zhao, Xinqing Li, Mohammed Shokr, Petra Heil, Jiechen Zhao, Lin Zhang, and Xiao Cheng. "Satellite-Based Sea Ice Navigation for Prydz Bay, East Antarctica." Remote Sensing 9, no. 6 (May 24, 2017): 518. http://dx.doi.org/10.3390/rs9060518.

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38

Broussard, Albert S., and Delores Nason McBroome. "Parallel Communities: African Americans in California's East Bay, 1850-1963." Western Historical Quarterly 25, no. 2 (1994): 222. http://dx.doi.org/10.2307/971471.

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39

Kaminuma, Katsutada, and Masaki Kanao. "Local Seismic Activity around the Lützow-Holm Bay, East Antarctica." Ocean and Polar Research 26, no. 3 (September 30, 2004): 523–29. http://dx.doi.org/10.4217/opr.2004.26.3.523.

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40

De Lange, Vincent P., and David L. Freitas. "DECHLORINATION SYSTEM IMPROVEMENTS AT THE EAST BAY MUNICIPAL UTILITY DISTRICT." Proceedings of the Water Environment Federation 2001, no. 15 (January 1, 2001): 544–54. http://dx.doi.org/10.2175/193864701790903067.

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41

Kraus, Nicholas C., and Adele Militello. "Hydraulic Study of Multiple Inlet System: East Matagorda Bay, Texas." Journal of Hydraulic Engineering 125, no. 3 (March 1999): 224–32. http://dx.doi.org/10.1061/(asce)0733-9429(1999)125:3(224).

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42

Johnson, Marilynn S. "War as Watershed: The East Bay and World War II." Pacific Historical Review 63, no. 3 (August 1, 1994): 315–31. http://dx.doi.org/10.2307/3640969.

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43

Zhao, Feiyu, Suhua Jiang, Sanzhong Li, Huixuan Zhang, Gang Wang, Jianping Lei, and Song Gao. "Cenozoic tectonic migration in the Bohai Bay Basin, East China." Geological Journal 51 (March 30, 2016): 188–202. http://dx.doi.org/10.1002/gj.2787.

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44

Yamane, Masako, Yusuke Yokoyama, Hideki Miura, Hideaki Maemoku, Shogo Iwasaki, and Hiroyuki Matsuzaki. "The last deglacial history of Lützow-Holm Bay, East Antarctica." Journal of Quaternary Science 26, no. 1 (January 2011): 3–6. http://dx.doi.org/10.1002/jqs.1465.

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Yang, Ruowen, Shu Gui, and Jie Cao. "Bay of Bengal‐East Asia‐Pacific Teleconnection in Boreal Summer." Journal of Geophysical Research: Atmospheres 124, no. 8 (April 26, 2019): 4395–412. http://dx.doi.org/10.1029/2019jd030332.

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46

Akamatsu, Junpei. "Coda attenuation in the Lützow-Holm Bay region, East Antarctica." Physics of the Earth and Planetary Interiors 67, no. 1-2 (May 1991): 65–75. http://dx.doi.org/10.1016/0031-9201(91)90060-u.

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47

SAMAAI, TOUFIEK, RUWEN PILLAY, and LIESL JANSON. "Shallow-water Demospongiae (Porifera) from Sodwana Bay, iSimangaliso Wetland Park, South Africa." Zootaxa 4587, no. 1 (April 23, 2019): 1. http://dx.doi.org/10.11646/zootaxa.4587.1.1.

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33 species of shallow-water Demospongiae (Phylum Porifera) are described from Sodwana Bay, iSimangaliso Wetland Park, on the east coast of South Africa. Of the 33 species collected, 18 are redescribed from fresh material and 15 are new to science. Orders Clionaida, Poecilosclerida, Axinellida, Haplosclerida and Dictyoceratida are well represented in the collection with 4 to 6 species each, with the first three groups appearing to have the greatest diversity on the east coast of South Africa. The east coast of South Africa appears to have a high abundance of poecilosclerid and dictyoceratid sponges. The results of this study underscore the importance of poecilosclerid and dictyoceratid sponge fauna of the east coast of South Africa, in terms of the potential for the continued discovery of new species.

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48

Frederick, J. B., E. J. Davies, P. G. Smith, D. Spancers, and T. J. Williams. "EXPLORATION OPPORTUNITIES, EAST COAST BASIN, NEW ZEALAND." APPEA Journal 40, no. 1 (2000): 39. http://dx.doi.org/10.1071/aj99003.

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The Westech-Orion Joint Venture holds onshore Petroleum Exploration Permit 38329 and offshore PEPs 38325, 38326 and 38333 in the East Coast Basin, New Zealand. The Joint Venture holds 24,117 km2 covering Hawkes Bay and the Wairarapa shelf.The Westech-Orion Joint Venture has drilled six exploratory wells and five appraisal wells in the onshore East Coast Basin over a two year period. All wells encountered significant gas shows, with two wells discovering hydrocarbons in potentially commercial volumes. Each well was drilled on the crest of a seismically mapped structure, characterised by asymmetric folding over a northwest dipping thrust fault.Prior to this drilling program, the reservoir potential of the Wairoa area was inferred to be dominated by turbidite sandstones of the Tunanui and Makaretu formations (Mid-Late Miocene). The new wells show that the Mid Miocene and parts of the Early and Late Miocene pinch out across the 'Wairoa High'.One of the primary onshore reservoirs is the Kauhauroa Limestone (Early Miocene), a bryozoan-dominated, tightly packed and cemented limestone with dominantly fracture porosity. The other primary reservoir is the Tunanui Sandstone (Mid Miocene), which in well intersections to date comprises medium-thickly bedded sandstone, with net sand typically 40%. The sands have high lithic content, and are moderately sorted and subangular-subrounded.Abnormally high formation pressures were encountered in all wells, ranging up to 3,400 psi at 1,000 m. Crestal pressure gradients commonly exceed 70% of the lithostatic pressure gradient, despite the relative proximity to outcrop. The overpressure may reflect relatively young uplift of fossil pressures, with insufficient time for pressure equilibration within a generally overpressured system.The prospectivity of the area has been highgraded by recent maturation and reservoir studies in Hawkes Bay and by gas discoveries in Westech-Orion wells onshore northern Hawkes Bay. Maturation studies identified nine kitchen areas with oil migration commencing in the Late Miocene. Seismic stratigraphy and correlation with onshore wells identified offshore submarine fan deposits of Eocene, Early Miocene, Mid Miocene and Pliocene age.A 594 km2 exploration 3D seismic survey was acquired in Hawke Bay in April 1999, and 685 km of 2D seismic were acquired in March 2000. Preliminary interpretation of the 3D survey has yielded five prospects, each covering 20–90 km2. One prospect is a lowstand fan identified by stacked mounding and bidirectional downlap, correlated with the onshore Mid Miocene Tunanui Sandstone. High amplitude seismic events of Mid-Late Miocene ages are inferred to be pulses of submarine fan development, in places associated with direct hydrocarbon indicators (DHIs). High amplitude seismic events in the Pliocene include a package of high amplitude seismic reflectors interpreted as structurally trapped DHI truncated by a major unconformity.

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Treloar, Philip, David Taylor, and Paul Prenzler. "INVESTIGATION OF WAVE INDUCED STORM SURGE WITHIN A LARGE COASTAL EMBAYMENT - MORETON BAY (AUSTRALIA)." Coastal Engineering Proceedings 1, no. 32 (January 30, 2011): 22. http://dx.doi.org/10.9753/icce.v32.currents.22.

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Moreton Bay is a large coastal embayment on the south-east Queensland coast which is surrounded by the urbanised areas of greater Brisbane on its western and southern shorelines. It is protected from the open coast by a number of islands, including South Stradbroke, North Stradbroke and Moreton Islands. Tropical cyclones occasionally track far enough south to cause significant damage to south-east Queensland due to flooding, winds, waves and elevated ocean water levels. Distant tropical cyclones which may be several hundred kilometres north of Moreton Bay have been known to cause storm surge, high waves and erosion inside Moreton Bay. These events generally do not generate gale force winds within Moreton Bay, but can generate large ocean swell waves. It has been identified that the wave conditions generated from distant cyclones can cause a variation in water levels inside Moreton Bay. A detailed study was undertaken to investigate the regional wave set-up process which affects Moreton Bay. The simulation of the residual water levels within Moreton Bay using a coupled hydrodynamic and wave model system developed for this study is considerably more accurate than applying a hydrodynamic model alone and explains water level anomalies that have a tidal frequency. The paper discusses the physical process of regional wave set-up inside a large embayment, analysis of observed residual water level and also the modelling study undertaken to quantify the influence of waves on storm tide levels inside Moreton Bay. The storm tide hazard study for the Moreton Bay Councils included the effects of regional wave set-up in the specification of design water levels.

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Bondarev, O. V. "Dimensional age characteristics of juveniles cod Gadus morhuaLinnaeus, 1958 and Pollachius virenssites (Linnaeus, 1958) in the coastal zone of the Barents Sea in July 2018." Transaction Kola Science Centre 11, no. 5-2020 (March 25, 2020): 12–17. http://dx.doi.org/10.37614/2307-5252.2020.11.5.002.

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Data on the length of juveniles Atlantic cod and pollock in the coast of the Barents Sea in July 2018 are presented. It was established that, compared with the previous period, the growth rate of fishincreased. In July 2018, juveniles Atlantic cod and pollock from the Kola Bay and East Murman lips are characterized by positive allometric growth. Older age groups of fish from the Kola Bay also have positive alometric growth, and negative in Zelenetskaya Bay.

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Journal articles on the topic 'East of Bay'

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