標(biāo)題: Titlebook: Carbon and Nutrient Fluxes in Continental Margins; A Global Synthesis Kon-Kee Liu,Larry Atkinson,Liana Talaue-McManus Book 2010 Springer-Ve [打印本頁(yè)] 作者: 能干 時(shí)間: 2025-3-21 16:34
書目名稱Carbon and Nutrient Fluxes in Continental Margins影響因子(影響力)
書目名稱Carbon and Nutrient Fluxes in Continental Margins影響因子(影響力)學(xué)科排名
書目名稱Carbon and Nutrient Fluxes in Continental Margins網(wǎng)絡(luò)公開度
書目名稱Carbon and Nutrient Fluxes in Continental Margins網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Carbon and Nutrient Fluxes in Continental Margins被引頻次
書目名稱Carbon and Nutrient Fluxes in Continental Margins被引頻次學(xué)科排名
書目名稱Carbon and Nutrient Fluxes in Continental Margins年度引用
書目名稱Carbon and Nutrient Fluxes in Continental Margins年度引用學(xué)科排名
書目名稱Carbon and Nutrient Fluxes in Continental Margins讀者反饋
書目名稱Carbon and Nutrient Fluxes in Continental Margins讀者反饋學(xué)科排名
作者: 獸群 時(shí)間: 2025-3-22 00:12
Positron Annihilation Spectroscopy (PAS),2005), Mackas et al. (2006), Fréon et al. (2006), and Taylor and Wolff (2007), compare eastern boundary current systems (EBCS) from physical, productivity, trophic, or biogeochemical standpoints. Therefore, this section focuses mostly on some key research areas that have begun to emerge in the last 作者: tenuous 時(shí)間: 2025-3-22 02:51
R. G. Thompson,C. J. Fiedler,O. Buck globally significant amounts of heat, nutrients, and carbon to higher latitudes. The movement of material and heat to higher latitudes has significant effects on the global climate but also significantly affects the ocean margin through which they pass.作者: Expediency 時(shí)間: 2025-3-22 05:31
https://doi.org/10.1007/978-1-4684-4769-9 and poorly understood oceanographically than the Atlantic and Pacific Oceans. The complexity owes to its peculiar geographical setting: its northern expanse is limited by land just north of the Tropic of Cancer. This has important consequences for both surface and subsurface circulations, the forme作者: landfill 時(shí)間: 2025-3-22 11:17
R. G. Thompson,C. J. Fiedler,O. Buckns is marked in the west of the ocean basins by the separation point of the major western boundary currents, and in the east by the more diffuse re-attachment of the westwind drift to the continental margin. We also include the landmass of New Zealand, situated within the path of both the South Paci作者: FANG 時(shí)間: 2025-3-22 15:15 作者: FANG 時(shí)間: 2025-3-22 19:04
https://doi.org/10.1007/978-1-4684-4769-9s (Liu et al. 2000a) and, as such, have been of considerable interest to the JGOFS and LOICZ (Chen et al. 1994). This chapter is devoted entirely to address marginal seas, defined as semi-enclosed seas adjacent to a continent. It provides a detailed discussion of the C/N/P fluxes for the Baltic, Bla作者: 我要威脅 時(shí)間: 2025-3-23 00:57
Maimunah Mohd Ali,Norhashila Hashimquently warmer than other parts of the earth. Higher solar energy inputs are about the only rational (but still contested) explanation for the orders of magnitude greater biological species diversity (Allen et al. 2002; Algar et al. 2006) and hydrological and biogeochemical cycling speeds observed i作者: 領(lǐng)先 時(shí)間: 2025-3-23 03:21
https://doi.org/10.1007/978-3-030-01899-3tal zone, the interphase domain between land, ocean, and atmosphere. The coast and its ecosystems, including wetlands, estuaries, marshes, mangroves, seagrasses, and coral reefs, are continuously modified by human activities through changing land and water uses, and increasing waste loading from eco作者: ALIEN 時(shí)間: 2025-3-23 05:59 作者: jungle 時(shí)間: 2025-3-23 11:01 作者: Insul島 時(shí)間: 2025-3-23 16:40
O. Büyük?ztürk,R. Haupt,C. Tuakta,J. Chenon budget and for developing and testing our understanding of processes that ultimately control these budgets. Continental margins are composed of the continental slope, shelf, and rise. These coastal regions are a crucial boundary between land and ocean, a focal point for the accumulation and trans作者: Hyaluronic-Acid 時(shí)間: 2025-3-23 19:18
Progress in Theoretical Computer Science, hydrosphere, lithosphere, and the biosphere. In the natural carbon cycle, the time period for the atmosphere–biosphere exchange is the shortest with a range of just a few months to a few decades. The atmosphere–hydrosphere exchange of CO., on the other hand, takes several 100 years if the interior作者: 保留 時(shí)間: 2025-3-23 22:10 作者: Grating 時(shí)間: 2025-3-24 03:57
Isaac Elishakoff,Lova Andriamasyution, the continental shelf sedimentation patterns formed during the Holocene period and the related processes are examined, the impact of sedimentary processes on carbon burial on the continental shelf is evaluated, and the scientific problems that need solutions for the future trends of sediment 作者: NATAL 時(shí)間: 2025-3-24 08:55 作者: 凈禮 時(shí)間: 2025-3-24 11:03
https://doi.org/10.1007/978-3-540-92735-8Biogeochemical fluxes; Carbon cycle; Coast; Coastal ocean; Continental shelves; Global change; IGBP; Indian作者: 階層 時(shí)間: 2025-3-24 15:49
978-3-662-51787-1Springer-Verlag Berlin Heidelberg 2010作者: cutlery 時(shí)間: 2025-3-24 19:12 作者: Pcos971 時(shí)間: 2025-3-25 01:30
Carbon and Nutrient Fluxes in Continental Margins978-3-540-92735-8Series ISSN 1619-2435 作者: relieve 時(shí)間: 2025-3-25 06:18 作者: 煞費(fèi)苦心 時(shí)間: 2025-3-25 09:38
Kon-Kee Liu,Larry Atkinson,Liana Talaue-McManusExcellent guide for researchers of all levels and for the study of graduate students.Includes supplementary material: 作者: 有惡意 時(shí)間: 2025-3-25 13:35
Global Change - The IGBP Serieshttp://image.papertrans.cn/c/image/221646.jpg作者: Slit-Lamp 時(shí)間: 2025-3-25 16:36
Biogeochemistry of Continental Margins in a Global Contextt attention given to continental margins focused on continental shelves, which constitute a major part of continental margins. In recent years, it has been increasingly appreciated that influences of the land–ocean boundary often extend beyond the shelf edge. Such new ideas have led to recognition o作者: CHASM 時(shí)間: 2025-3-25 23:54
Eastern Boundary Current Systems2005), Mackas et al. (2006), Fréon et al. (2006), and Taylor and Wolff (2007), compare eastern boundary current systems (EBCS) from physical, productivity, trophic, or biogeochemical standpoints. Therefore, this section focuses mostly on some key research areas that have begun to emerge in the last 作者: 斗志 時(shí)間: 2025-3-26 01:58
Western Boundary Currents globally significant amounts of heat, nutrients, and carbon to higher latitudes. The movement of material and heat to higher latitudes has significant effects on the global climate but also significantly affects the ocean margin through which they pass.作者: PANEL 時(shí)間: 2025-3-26 08:02 作者: lymphoma 時(shí)間: 2025-3-26 10:51
Subpolar Marginsns is marked in the west of the ocean basins by the separation point of the major western boundary currents, and in the east by the more diffuse re-attachment of the westwind drift to the continental margin. We also include the landmass of New Zealand, situated within the path of both the South Paci作者: 任意 時(shí)間: 2025-3-26 12:40 作者: BURSA 時(shí)間: 2025-3-26 17:49 作者: peritonitis 時(shí)間: 2025-3-26 23:50 作者: 松馳 時(shí)間: 2025-3-27 03:12 作者: expository 時(shí)間: 2025-3-27 06:36
Biogeochemical Transformations of Silicon Along the Land–Ocean Continuum and Implications for the Glely changes as consequence of global changes. Largescale programs investigated the oceanic cycling of carbon (C) and associated biogenic elements, mainly nitrogen (N) and phosphorus (P), as limiting nutrients of the global production by marine phytoplankton (Falkowski 1997; Tyrrell 1999). However, c作者: clarify 時(shí)間: 2025-3-27 09:46 作者: NICHE 時(shí)間: 2025-3-27 13:56
Coupled Circulation/Biogeochemical Models to Estimate Carbon Flux1on budget and for developing and testing our understanding of processes that ultimately control these budgets. Continental margins are composed of the continental slope, shelf, and rise. These coastal regions are a crucial boundary between land and ocean, a focal point for the accumulation and trans作者: 短程旅游 時(shí)間: 2025-3-27 17:53 作者: 支架 時(shí)間: 2025-3-27 23:55 作者: 行業(yè) 時(shí)間: 2025-3-28 04:39
Sediment and Carbon Accumulation on Continental Shelves1ution, the continental shelf sedimentation patterns formed during the Holocene period and the related processes are examined, the impact of sedimentary processes on carbon burial on the continental shelf is evaluated, and the scientific problems that need solutions for the future trends of sediment 作者: 突襲 時(shí)間: 2025-3-28 07:19 作者: 傳授知識(shí) 時(shí)間: 2025-3-28 13:59 作者: 丑惡 時(shí)間: 2025-3-28 17:39
https://doi.org/10.1007/978-3-662-08988-0 been increasingly appreciated that influences of the land–ocean boundary often extend beyond the shelf edge. Such new ideas have led to recognition of the significance of continental margins in the earth system. The studies have enabled a more quantitative depiction of biogeochemical cycles in continental margins, which is presented in this book.作者: 山崩 時(shí)間: 2025-3-28 21:19
Positron Annihilation Spectroscopy (PAS),vity, trophic, or biogeochemical standpoints. Therefore, this section focuses mostly on some key research areas that have begun to emerge in the last few years and that are essential for understanding the structure and function of EBCS.作者: 全部逛商店 時(shí)間: 2025-3-28 23:26
R. G. Thompson,C. J. Fiedler,O. Bucktachment of the westwind drift to the continental margin. We also include the landmass of New Zealand, situated within the path of both the South Pacific west wind drift and the eastward flow associated with the subtropical convergence.作者: 龍蝦 時(shí)間: 2025-3-29 06:14
https://doi.org/10.1007/978-1-4684-4769-9ddress marginal seas, defined as semi-enclosed seas adjacent to a continent. It provides a detailed discussion of the C/N/P fluxes for the Baltic, Black, East (Sea of Japan), Mediterranean, North, and Okhotsk Seas, as well as the Mississippi River plume and the adjacent margin in the Gulf of Mexico.作者: 拾落穗 時(shí)間: 2025-3-29 09:43 作者: myriad 時(shí)間: 2025-3-29 13:03
Eastern Boundary Current Systemsvity, trophic, or biogeochemical standpoints. Therefore, this section focuses mostly on some key research areas that have begun to emerge in the last few years and that are essential for understanding the structure and function of EBCS.作者: EXUDE 時(shí)間: 2025-3-29 18:06
Subpolar Marginstachment of the westwind drift to the continental margin. We also include the landmass of New Zealand, situated within the path of both the South Pacific west wind drift and the eastward flow associated with the subtropical convergence.作者: Incisor 時(shí)間: 2025-3-29 22:10
Marginal Seasddress marginal seas, defined as semi-enclosed seas adjacent to a continent. It provides a detailed discussion of the C/N/P fluxes for the Baltic, Black, East (Sea of Japan), Mediterranean, North, and Okhotsk Seas, as well as the Mississippi River plume and the adjacent margin in the Gulf of Mexico.作者: precede 時(shí)間: 2025-3-30 02:14
Book 2010 Team which was established to facilitate continental margins research in the two projects. It contains signi cant information on the physical, biogeochemical, and ecosystems of continental margins nationally and regionally and provides a very valuable synthesis of this information and the physical,作者: Evocative 時(shí)間: 2025-3-30 05:51
Small Angle Neutron Scattering an NDE Tooltrol the carbon cycle and fluxes of each region. Yet because of their polar nature, there also are similarities in physical forcing which can drive the chemical, biological and geological processes that influence the biogeochemical cycles of the regions.作者: 額外的事 時(shí)間: 2025-3-30 10:52
https://doi.org/10.1007/978-94-007-0723-8undwater discharge may be equally or even more important in terms of material transport across land/sea margins (Li et al. 1999; Kim et al. 2002; Burnett 2003; Kim et al. 2003a). In this chapter, we therefore define SGD to consist truly fresh groundwater, recirculated seawater, or a composite thereof.作者: 拱形大橋 時(shí)間: 2025-3-30 14:24 作者: 友好 時(shí)間: 2025-3-30 16:52
Isaac Elishakoff,Lova Andriamasytion rate. The burial of organic carbon is associated with fine-grained sediment, which covers about 22% of the area of the world’s shelf regions, while the burial of inorganic carbon takes place not only in fine-grained sediments but also in relict sediments, shell beds, and coral reefs on the shelf.作者: Common-Migraine 時(shí)間: 2025-3-30 22:32
Submarine Groundwater Discharge (SGD) and Associated Nutrient Fluxes to the Coastal Oceanundwater discharge may be equally or even more important in terms of material transport across land/sea margins (Li et al. 1999; Kim et al. 2002; Burnett 2003; Kim et al. 2003a). In this chapter, we therefore define SGD to consist truly fresh groundwater, recirculated seawater, or a composite thereof.作者: 翻動(dòng) 時(shí)間: 2025-3-31 02:24
Cross-Boundary Exchanges of Carbon and Nitrogen in Continental Margins1se surface waters, whether terrestrial or oceanic, generally reach an equilibrium with atmospheric CO. and other gases somewhat rapidly. By contrast, it takes several 100 years for the surface waters of the oceans to first sink to great depths in the polar regions, and then slowly move horizontally to fill in the deep basins of the world’s oceans.作者: 支架 時(shí)間: 2025-3-31 06:55
Sediment and Carbon Accumulation on Continental Shelves1tion rate. The burial of organic carbon is associated with fine-grained sediment, which covers about 22% of the area of the world’s shelf regions, while the burial of inorganic carbon takes place not only in fine-grained sediments but also in relict sediments, shell beds, and coral reefs on the shelf.作者: 最初 時(shí)間: 2025-3-31 09:43 作者: fodlder 時(shí)間: 2025-3-31 14:15 作者: Microgram 時(shí)間: 2025-3-31 20:47
Global Synthesis1astal or margin dimensions (e.g., distance from the shoreline to the 130m isobath; Wollast 1998; Mackenzie et al. 2004). However, many important transport processes that are directly associated with the margin often extend across these depth boundaries and the resulting budgets may not fully represent the role of margins in biogeochemical cycles.作者: Ardent 時(shí)間: 2025-3-31 22:06 作者: 瑣事 時(shí)間: 2025-4-1 02:19 作者: Bronchial-Tubes 時(shí)間: 2025-4-1 07:45 作者: 拒絕 時(shí)間: 2025-4-1 11:10
NDT Geophysical Data Interpretation,tinental margins, their contribution to carbon dioxide (CO.) sequestration and to determine horizontal C and associated biogenic element fluxes, some 200 N and P flux budgets have been constructed around the world (cf. Smith et al. 2003b, LOICZ 1998). One biogenic element, silicon (Si) has been larg
