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Gotowe bibliografie tematyczne / Botany Bay Region (N.S.W.)

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Artykuły w czasopismach

Gotowa bibliografia na temat „Botany Bay Region (N.S.W.)”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 14 lutego 2022

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Artykuły w czasopismach na temat "Botany Bay Region (N.S.W.)"

1

Yakubu, Bashir Ishaku, Shua’ib Musa Hassan, and Sallau Osisiemo Asiribo. "AN ASSESSMENT OF SPATIAL VARIATION OF LAND SURFACE CHARACTERISTICS OF MINNA, NIGER STATE NIGERIA FOR SUSTAINABLE URBANIZATION USING GEOSPATIAL TECHNIQUES." Geosfera Indonesia 3, no. 2 (August 28, 2018): 27. http://dx.doi.org/10.19184/geosi.v3i2.7934.

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Rapid urbanization rates impact significantly on the nature of Land Cover patterns of the environment, which has been evident in the depletion of vegetal reserves and in general modifying the human climatic systems (Henderson, et al., 2017; Kumar, Masago, Mishra, & Fukushi, 2018; Luo and Lau, 2017). This study explores remote sensing classification technique and other auxiliary data to determine LULCC for a period of 50 years (1967-2016). The LULCC types identified were quantitatively evaluated using the change detection approach from results of maximum likelihood classification algorithm

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2

Miranda, Luiz Bruner de, Ilson Carlos Almeida da Silveira, Felipe Pires Alvarenga Fernandes, Leandro Ponsoni, and Thiago Podadera Costa. "A descriptive analysis of the seasonal variation of physical oceanographic characteristics in the northern region of the Todos os Santos Bay (Bahia, Brazil)." Brazilian Journal of Oceanography 59, no. 1 (March 2011): 9–26. http://dx.doi.org/10.1590/s1679-87592011000100002.

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The results obtained in the August and December 2003, August 2004 and January 2005 oceanographic campaigns in the northern region of the Todos os Santos Bay (lat. 12º44.5'S; long. 038º35.00'W) between the Madre de Deus and Maré islands are analyzed. Instruments of continuous and discrete samplings were used to measure hydrographic properties currents and tides. The water mass of the northern region of the bay is forced by semidiurnal and mesotides of form number 0.08 and the lunar component M2 height was estimated at 91cm. The time series of the surface currents indicated movements in the N/S

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3

Wentworth, G. R., J. G. Murphy, B. Croft, R. V. Martin, J. R. Pierce, J. S. Côté, I. Courchesne, et al. "Ammonia in the summertime Arctic marine boundary layer: sources, sinks and implications." Atmospheric Chemistry and Physics Discussions 15, no. 21 (November 2, 2015): 29973–30016. http://dx.doi.org/10.5194/acpd-15-29973-2015.

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Abstract. Continuous hourly measurements of gas-phase ammonia (NH3(g)) were taken from 13 July to 7 August 2014 on a research cruise throughout Baffin Bay and the eastern Canadian Arctic Archipelago. Concentrations ranged from 30–650 ng m−3 (40–870 pptv) with the highest values recorded in Lancaster Sound (74°13' N, 84°00' W). Simultaneous measurements of total ammonium ([NHx]), pH and temperature in the ocean and in melt ponds were used to compute the compensation point (χ), which is the ambient NH3(g) concentration at which surface–air fluxes change direction. Ambient NH3(g) was usually seve

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4

Wentworth, Gregory R., Jennifer G. Murphy, Betty Croft, Randall V. Martin, Jeffrey R. Pierce, Jean-Sébastien Côté, Isabelle Courchesne, et al. "Ammonia in the summertime Arctic marine boundary layer: sources, sinks, and implications." Atmospheric Chemistry and Physics 16, no. 4 (February 22, 2016): 1937–53. http://dx.doi.org/10.5194/acp-16-1937-2016.

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Abstract. Continuous hourly measurements of gas-phase ammonia (NH3(g)) were taken from 13 July to 7 August 2014 on a research cruise throughout Baffin Bay and the eastern Canadian Arctic Archipelago. Concentrations ranged from 30 to 650 ng m−3 (40–870 pptv) with the highest values recorded in Lancaster Sound (74°13′ N, 84°00′ W). Simultaneous measurements of total ammonium ([NHx]), pH and temperature in the ocean and in melt ponds were used to compute the compensation point (χ), which is the ambient NH3(g) concentration at which surface–air fluxes change direction. Ambient NH3(g) was usually s

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5

Fadnavis, Suvarna, Gayatry Kalita, K. Ravi Kumar, Blaž Gasparini, and Jui-Lin Frank Li. "Potential impact of carbonaceous aerosol on the upper troposphere and lower stratosphere (UTLS) and precipitation during Asian summer monsoon in a global model simulation." Atmospheric Chemistry and Physics 17, no. 18 (September 28, 2017): 11637–54. http://dx.doi.org/10.5194/acp-17-11637-2017.

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Abstract. Recent satellite observations show efficient vertical transport of Asian pollutants from the surface to the upper-level anticyclone by deep monsoon convection. In this paper, we examine the transport of carbonaceous aerosols, including black carbon (BC) and organic carbon (OC), into the monsoon anticyclone using of ECHAM6-HAM, a global aerosol climate model. Further, we investigate impacts of enhanced (doubled) carbonaceous aerosol emissions on the upper troposphere and lower stratosphere (UTLS), underneath monsoon circulation and precipitation from sensitivity simulations. The model

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6

George, Jenson V., P. N. Vinayachandran, V. Vijith, V. Thushara, Anoop A. Nayak, Shrikant M. Pargaonkar, P. Amol, K. Vijaykumar, and Adrian J. Matthews. "Mechanisms of Barrier Layer Formation and Erosion from In Situ Observations in the Bay of Bengal." Journal of Physical Oceanography 49, no. 5 (May 2019): 1183–200. http://dx.doi.org/10.1175/jpo-d-18-0204.1.

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AbstractDuring the Bay of Bengal (BoB) Boundary Layer Experiment (BoBBLE) in the southern BoB, time series of microstructure measurements were obtained at 8°N, 89°E from 4 to 14 July 2016. These observations captured events of barrier layer (BL) erosion and reformation. Initially, a three-layer structure was observed: a fresh surface mixed layer (ML) of thickness 10–20 m; a BL below of 30–40-m thickness with similar temperature but higher salinity; and a high salinity core layer, associated with the Summer Monsoon Current. Each of these three layers was in relative motion to the others, leadin

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7

Pasteur, E. C., R. Mulvaney, D. A. Peel, E. S. Saltzman, and P.-Y. Whung. "A 340 year record of biogenic sulphur from the Weddell Sea area, Antarctica." Annals of Glaciology 21 (1995): 169–74. http://dx.doi.org/10.1017/s0260305500015779.

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Detailed records of methanesulphonic acid (MSA) and non-sea-salt sulphate (nss SO4 2−) have been obtained from ice cores drilled on Dolleman Island on the east coast of the Antarctic Peninsula (70°35.2′S, 60°55.5′W). Annual average concentrations of MSA are presented for the period 1652–1992. Over this time span, the mean annual concentration of MSA is 0.69 μeq l−1 (σ = 0.33, n = 340), the range is 0.13–2.35μeq l−1, and the MSA/nss-SO4 2− ratio is 0.22. The high MSA concentration reflects the proximity of the Weddell Sea, believed to be a region of high marine phytoplankton production. The ove

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8

Pasteur, E. C., R. Mulvaney, D. A. Peel, E. S. Saltzman, and P.-Y. Whung. "A 340 year record of biogenic sulphur from the Weddell Sea area, Antarctica." Annals of Glaciology 21 (1995): 169–74. http://dx.doi.org/10.3189/s0260305500015779.

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Detailed records of methanesulphonic acid (MSA) and non-sea-salt sulphate (nss SO42−) have been obtained from ice cores drilled on Dolleman Island on the east coast of the Antarctic Peninsula (70°35.2′S, 60°55.5′W). Annual average concentrations of MSA are presented for the period 1652–1992. Over this time span, the mean annual concentration of MSA is 0.69 μeq l−1 (σ = 0.33, n = 340), the range is 0.13–2.35μeq l−1, and the MSA/nss-SO42− ratio is 0.22. The high MSA concentration reflects the proximity of the Weddell Sea, believed to be a region of high marine phytoplankton production. The overa

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9

Biays, Pierre. "Le courant du Labrador et quelques-unes de ses conséquences géographiques." Cahiers de géographie du Québec 4, no. 8 (April 12, 2005): 237–301. http://dx.doi.org/10.7202/020220ar.

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I. A part of the West Greenland current flows westwards across the Davis Strait and meets the Canadian (Baffin Land) current to form the Labrador current which follows southwards the shelf and slope of Labrador Coast {figure I). Meeting the northern edge of the Newfoundland Banks, the Labrador current splits in a minor western branch running along the Avalon Peninsula and a major one proceeding south along the eastern edge of the shelf down to the Tail of the Grand Banks. There it meets the Atlantic current which very often forms a prominent westward salient at about 45°N. and 47 - 48°W. (figu

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10

Park, M. J., S. E. Cho, M. Piątek, and H. D. Shin. "First Report of Powdery Mildew Caused by Erysiphe macleayae on Macleaya microcarpa in Poland." Plant Disease 96, no. 9 (September 2012): 1376. http://dx.doi.org/10.1094/pdis-03-12-0244-pdn.

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Macleaya microcarpa (Maxim.) Fedde, also known as smallfruit plume poppy, is a perennial herb belonging to the family Papaveraceae. The plant, together with the better-known species M. cordata (Willd.) R. Br., is native to central China and is now planted worldwide for medicinal purposes. In October 2008 and August 2009, dozens of smallfruit plume poppy planted in the Kraków Botanical Garden, Poland, were found to be severely infected with a powdery mildew. White colonies with abundant sporulation developed on both sides of leaves and young stems, forming circular to irregular patches. Infecti

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