NSTL国家科技图书文献中心

1. The Impact of Anomalous Biomass Burning on Phytoplankton and Surface Ocean Carbon Pool in the Indo-China Peninsula NSTL国家科技图书文献中心

Liu, Wenjing | Wang, Wencai - 《Journal of Geophysical Research,C.Oceans》 - 2025,130(3) - n/a～n/a - 共19页

摘要： to the expansion of the surface ocean carbon pool | the surface* ocean carbon pool by 2.64 x 107 kg* | The ocean* carbon sink plays a pivotal role in* | , there was no significant increase in ocean carbon | export. Ultimately, the response of the surface ocean

关键词： chlorophyll-a concentrations | surface ocean carbon pool | biomass burning | Indo-China Peninsula

2. Size-fractionated C:N:P:Si stoichiometry of particulate matter in the subtropical Western North Pacific NSTL国家科技图书文献中心

Wang, Chaoyong | Zhang, Kan ... - 《Global and planetary change》 - 2025,246(Mar.) - 1.1～1.14 - 共14页

摘要： variations in the upper ocean* are crucial for understanding* | carbon export and its coupling with nutrient dynamics | particulate organic carbon* (POC), particulate nitrogen (PN* | PP concentrations consistently occurred in surface | ) dominated the total pool* of POC, PN, and PP but*

关键词： C:N:P:Si stoichiometry | size-fractionated biogenic particles | phytoplankton community composition | subtropical western North Pacific | ELEMENTAL STOICHIOMETRY | ORGANIC-MATTER | ECOLOGICAL STOICHIOMETRY | MARINE PROCHLOROCOCCUS | SCALE VARIATIONS | SURFACE OCEAN...

3. Seasonal and Interannual Variability of Particulate Organic Carbon in the Banda Sea NSTL国家科技图书文献中心

Jia, Yijia | Wang, Zhenyan ... - 《Journal of Geophysical Research,C.Oceans》 - 2025,130(5) - n/a～n/a - 共21页

摘要： of the Indo-Pacific Warm Pool, the Banda Sea is | variability and control mechanism of surface* particulate* | organic carbon* (POC) in the Banda Sea. Using 19 years of* | spatial and temporal variability of surface* POC. A self* | surface currents. Concentrations of POC are higher in

关键词： particulate organic carbon | upwelling | South China Sea throughflow | Banda Sea | El Ni & ntilde;o-Southern Oscillation (ENSO) | Indian Ocean Dipole (IOD)

4. Inconsistent Fast and Slow Responses of East Asian Summer Monsoon Precipitation Forced by Black Carbon NSTL国家科技图书文献中心

Fang, Chenwei | Zhu, Bin ... - 《Journal of Climate》 - 2025,38(4) - 1081～1103 - 共23页

摘要：, teeming with anthropogenic black carbon* (BC), lacks* | slow sea surface* temperature (SST)-meditated* | southwesterlies, primarily from tropical Indian Ocean, overweigh | those of surface* evaporation changes, governing both* | -induced SST warming in the Indo-Pacific warm pool

关键词： Monsoons | Precipitation | Anthropogenic effects/forcing | Water vapor | Aerosols/particulates | Air-sea interaction

5. Variable aging and storage of dissolved black carbon in the ocean NSTL国家科技图书文献中心

Alysha I. Coppola | Ellen R. M. Druffe ... - 《Proceedings of the National Academy of Sciences of the United States of America.》 - 2024,121(13) - e2305030121～e2305030121 - 共6页

摘要： carbon (DOC) pool. The fate of BC is considered to | pool of organic carbon in the oceans, yet most DOC | , biomass is converted to black carbon* (BC) via incomplete* | combustion. BC enters the ocean* by rivers and atmospheric* | reside in the marine DOC pool, where the oldest BC 14C

关键词： dissolved organic carbon | dissolved black carbon | ocean carbon cycle | refractory and semilabile DOC | size-fractionated DOC

6. Editorial preface to special issue: Neogene-Quaternary changes of the Indo-Pacific Warm Pool encompassing oceanic, hydrologic and carbon cycles, and their implications for future change NSTL国家科技图书文献中心

Huang J. | Xiong Z.... - 《Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences》 - 2024,642 - 共5页

摘要： processes via the ocean water-column, sea surface | © 2024 Elsevier B.V.The Indo-Pacific Warm Pool | addressing two primary themes: (1) Ocean-atmosphere coupled | source-to-sink and biogeochemical carbon-cycles, and | , salinity, oxygenation, hydrography, carbon* cycle*

关键词： Indo-Pacific Warm Pool | Paleoceanography | Paleoclimate

7. The impact of eddies and spring warm pool on sinking rates of phytoplankton with different shapes and sizes NSTL国家科技图书文献中心

Yingjie Mao | Congcong Guo ... - 《Marine Biology: International Journal on Life in Oceans and Coastal Waters》 - 2024,171(5) - 1.1～1.22 - 共22页

摘要： surface seawater are proven to be one of the major | contributors to the mesopelagic carbon* flux. Phytoplankton* | carbon biomass and sinking fluxes. Here, we measured | ), warm eddy (WE) and spring warm pool* (SWP), and* | the influence of SWP, with the highest carbon* fluxes*

关键词： Phytoplankton sinking rates | Luzon cold eddy | Warm eddy | Spring warm pool | Cell shapes | Cell size

8. pH Distributions and Determining Processes Along the U.S. East Coast NSTL国家科技图书文献中心

Xinyu Li | Yuan‐Yuan Xu ... - 《Journal of Geophysical Research, C. Oceans: JGR》 - 2024,129(9) - n/a～n/a - 共20页

摘要：Abstract pH is a key index in ocean | associated with the Cold Pool* water, and an inflow of low* | prominent role in regulating sea‐surface* pHT, driving it* | the pHT decrease caused by the anthropogenic carbon | to processes such as water masses shifting, ocean

关键词： pH distribution | inorganic carbon system | U.S. East Coast | ocean acidification

9. Carbon Dynamics in a Changing Arctic Landscape: Characterizing Dissolved Organic Matter Across Multiple Scales NSTL国家科技图书文献中心

Starr, Sommer Faith. - Biogeochemistry.;Env... - Ph.D. - Spencer, Robert G. M... - 2024, - 1～198 - 共198页

摘要： DOM pool* rivaling the amount of carbon stored in the* | carbon cycles, transporting organic matter from | ecosystems on land to the Arctic Ocean. However, polar | releasing hundreds of tons of carbon* currently stored in* | surface waters. Dissolved organic matter (DOM) is a

关键词： Arctic biogeochemistry | Dissolved organic matter | Peatlands | Permafrost | Surface water

10. Suspended particles are hotspots of microbial remineralization in the ocean's twilight zone NSTL国家科技图书文献中心

V. Hemsley | J. Fuessel ... - 《Deep-sea research, Part II. Topical studies in oceanography》 - 2023,212(Dec.) - 105339.1～105339.13 - 共13页

摘要： organic carbon* from the ocean surface to its interior is* | exerting control over ocean-atmosphere carbon* dioxide* | , resulting in rapid turnover of the suspended carbon pool | a significant term in the global carbon* cycle* | . Most sinking organic carbon* is, however*

摘要： to the expansion of the surface ocean carbon pool | the surface* ocean carbon pool by 2.64 x 107 kg* | The ocean* carbon sink plays a pivotal role in* | , there was no significant increase in ocean carbon | export. Ultimately, the response of the surface ocean

关键词： chlorophyll-a concentrations | surface ocean carbon pool | biomass burning | Indo-China Peninsula

摘要： variations in the upper ocean* are crucial for understanding* | carbon export and its coupling with nutrient dynamics | particulate organic carbon* (POC), particulate nitrogen (PN* | PP concentrations consistently occurred in surface | ) dominated the total pool* of POC, PN, and PP but*

关键词： C:N:P:Si stoichiometry | size-fractionated biogenic particles | phytoplankton community composition | subtropical western North Pacific | ELEMENTAL STOICHIOMETRY | ORGANIC-MATTER | ECOLOGICAL STOICHIOMETRY | MARINE PROCHLOROCOCCUS | SCALE VARIATIONS | SURFACE OCEAN...

摘要： of the Indo-Pacific Warm Pool, the Banda Sea is | variability and control mechanism of surface* particulate* | organic carbon* (POC) in the Banda Sea. Using 19 years of* | spatial and temporal variability of surface* POC. A self* | surface currents. Concentrations of POC are higher in

关键词： particulate organic carbon | upwelling | South China Sea throughflow | Banda Sea | El Ni & ntilde;o-Southern Oscillation (ENSO) | Indian Ocean Dipole (IOD)

摘要：, teeming with anthropogenic black carbon* (BC), lacks* | slow sea surface* temperature (SST)-meditated* | southwesterlies, primarily from tropical Indian Ocean, overweigh | those of surface* evaporation changes, governing both* | -induced SST warming in the Indo-Pacific warm pool

关键词： Monsoons | Precipitation | Anthropogenic effects/forcing | Water vapor | Aerosols/particulates | Air-sea interaction

摘要： carbon (DOC) pool. The fate of BC is considered to | pool of organic carbon in the oceans, yet most DOC | , biomass is converted to black carbon* (BC) via incomplete* | combustion. BC enters the ocean* by rivers and atmospheric* | reside in the marine DOC pool, where the oldest BC 14C

关键词： dissolved organic carbon | dissolved black carbon | ocean carbon cycle | refractory and semilabile DOC | size-fractionated DOC

摘要： processes via the ocean water-column, sea surface | © 2024 Elsevier B.V.The Indo-Pacific Warm Pool | addressing two primary themes: (1) Ocean-atmosphere coupled | source-to-sink and biogeochemical carbon-cycles, and | , salinity, oxygenation, hydrography, carbon* cycle*

关键词： Indo-Pacific Warm Pool | Paleoceanography | Paleoclimate

摘要： surface seawater are proven to be one of the major | contributors to the mesopelagic carbon* flux. Phytoplankton* | carbon biomass and sinking fluxes. Here, we measured | ), warm eddy (WE) and spring warm pool* (SWP), and* | the influence of SWP, with the highest carbon* fluxes*

关键词： Phytoplankton sinking rates | Luzon cold eddy | Warm eddy | Spring warm pool | Cell shapes | Cell size

摘要：Abstract pH is a key index in ocean | associated with the Cold Pool* water, and an inflow of low* | prominent role in regulating sea‐surface* pHT, driving it* | the pHT decrease caused by the anthropogenic carbon | to processes such as water masses shifting, ocean

关键词： pH distribution | inorganic carbon system | U.S. East Coast | ocean acidification

摘要： DOM pool* rivaling the amount of carbon stored in the* | carbon cycles, transporting organic matter from | ecosystems on land to the Arctic Ocean. However, polar | releasing hundreds of tons of carbon* currently stored in* | surface waters. Dissolved organic matter (DOM) is a

关键词： Arctic biogeochemistry | Dissolved organic matter | Peatlands | Permafrost | Surface water

摘要： organic carbon* from the ocean surface to its interior is* | exerting control over ocean-atmosphere carbon* dioxide* | , resulting in rapid turnover of the suspended carbon pool | a significant term in the global carbon* cycle* | . Most sinking organic carbon* is, however*

关键词： Carbon cycling | Microbial respiration | Suspended particles | Dissolved organic matter | Chemoautotrophic

4008-161-200 800-990-8900

国家科技图书文献中心

摘要： to the expansion of the surface ocean carbon pool | the surface ocean carbon pool by 2.64 x 107 kg | The ocean carbon sink plays a pivotal role in | , there was no significant increase in ocean carbon | export. Ultimately, the response of the surface ocean

关键词： chlorophyll-a concentrations | surface ocean carbon pool | biomass burning | Indo-China Peninsula

摘要： variations in the upper ocean are crucial for understanding | carbon export and its coupling with nutrient dynamics | particulate organic carbon (POC), particulate nitrogen (PN | PP concentrations consistently occurred in surface | ) dominated the total pool of POC, PN, and PP but

关键词： C:N:P:Si stoichiometry | size-fractionated biogenic particles | phytoplankton community composition | subtropical western North Pacific | ELEMENTAL STOICHIOMETRY | ORGANIC-MATTER | ECOLOGICAL STOICHIOMETRY | MARINE PROCHLOROCOCCUS | SCALE VARIATIONS | SURFACE OCEAN...

摘要： of the Indo-Pacific Warm Pool, the Banda Sea is | variability and control mechanism of surface particulate | organic carbon (POC) in the Banda Sea. Using 19 years of | spatial and temporal variability of surface POC. A self | surface currents. Concentrations of POC are higher in

关键词： particulate organic carbon | upwelling | South China Sea throughflow | Banda Sea | El Ni & ntilde;o-Southern Oscillation (ENSO) | Indian Ocean Dipole (IOD)

摘要：, teeming with anthropogenic black carbon (BC), lacks | slow sea surface temperature (SST)-meditated | southwesterlies, primarily from tropical Indian Ocean, overweigh | those of surface evaporation changes, governing both | -induced SST warming in the Indo-Pacific warm pool

关键词： Monsoons | Precipitation | Anthropogenic effects/forcing | Water vapor | Aerosols/particulates | Air-sea interaction

摘要： carbon (DOC) pool. The fate of BC is considered to | pool of organic carbon in the oceans, yet most DOC | , biomass is converted to black carbon (BC) via incomplete | combustion. BC enters the ocean by rivers and atmospheric | reside in the marine DOC pool, where the oldest BC 14C

关键词： dissolved organic carbon | dissolved black carbon | ocean carbon cycle | refractory and semilabile DOC | size-fractionated DOC

摘要： processes via the ocean water-column, sea surface | © 2024 Elsevier B.V.The Indo-Pacific Warm Pool | addressing two primary themes: (1) Ocean-atmosphere coupled | source-to-sink and biogeochemical carbon-cycles, and | , salinity, oxygenation, hydrography, carbon cycle

关键词： Indo-Pacific Warm Pool | Paleoceanography | Paleoclimate

摘要： surface seawater are proven to be one of the major | contributors to the mesopelagic carbon flux. Phytoplankton | carbon biomass and sinking fluxes. Here, we measured | ), warm eddy (WE) and spring warm pool (SWP), and | the influence of SWP, with the highest carbon fluxes

关键词： Phytoplankton sinking rates | Luzon cold eddy | Warm eddy | Spring warm pool | Cell shapes | Cell size

摘要：Abstract pH is a key index in ocean | associated with the Cold Pool water, and an inflow of low | prominent role in regulating sea‐surface pHT, driving it | the pHT decrease caused by the anthropogenic carbon | to processes such as water masses shifting, ocean

关键词： pH distribution | inorganic carbon system | U.S. East Coast | ocean acidification

摘要： DOM pool rivaling the amount of carbon stored in the | carbon cycles, transporting organic matter from | ecosystems on land to the Arctic Ocean. However, polar | releasing hundreds of tons of carbon currently stored in | surface waters. Dissolved organic matter (DOM) is a

关键词： Arctic biogeochemistry | Dissolved organic matter | Peatlands | Permafrost | Surface water

摘要： organic carbon from the ocean surface to its interior is | exerting control over ocean-atmosphere carbon dioxide | , resulting in rapid turnover of the suspended carbon pool | a significant term in the global carbon cycle | . Most sinking organic carbon is, however

关键词： Carbon cycling | Microbial respiration | Suspended particles | Dissolved organic matter | Chemoautotrophic

4008-161-200 800-990-8900

国家科技图书文献中心

摘要： to the expansion of the surface ocean carbon pool | the surface* ocean carbon pool by 2.64 x 107 kg* | The ocean* carbon sink plays a pivotal role in* | , there was no significant increase in ocean carbon | export. Ultimately, the response of the surface ocean

摘要： variations in the upper ocean* are crucial for understanding* | carbon export and its coupling with nutrient dynamics | particulate organic carbon* (POC), particulate nitrogen (PN* | PP concentrations consistently occurred in surface | ) dominated the total pool* of POC, PN, and PP but*

摘要： of the Indo-Pacific Warm Pool, the Banda Sea is | variability and control mechanism of surface* particulate* | organic carbon* (POC) in the Banda Sea. Using 19 years of* | spatial and temporal variability of surface* POC. A self* | surface currents. Concentrations of POC are higher in

摘要：, teeming with anthropogenic black carbon* (BC), lacks* | slow sea surface* temperature (SST)-meditated* | southwesterlies, primarily from tropical Indian Ocean, overweigh | those of surface* evaporation changes, governing both* | -induced SST warming in the Indo-Pacific warm pool

摘要： carbon (DOC) pool. The fate of BC is considered to | pool of organic carbon in the oceans, yet most DOC | , biomass is converted to black carbon* (BC) via incomplete* | combustion. BC enters the ocean* by rivers and atmospheric* | reside in the marine DOC pool, where the oldest BC 14C

摘要： processes via the ocean water-column, sea surface | © 2024 Elsevier B.V.The Indo-Pacific Warm Pool | addressing two primary themes: (1) Ocean-atmosphere coupled | source-to-sink and biogeochemical carbon-cycles, and | , salinity, oxygenation, hydrography, carbon* cycle*

摘要： surface seawater are proven to be one of the major | contributors to the mesopelagic carbon* flux. Phytoplankton* | carbon biomass and sinking fluxes. Here, we measured | ), warm eddy (WE) and spring warm pool* (SWP), and* | the influence of SWP, with the highest carbon* fluxes*

摘要：Abstract pH is a key index in ocean | associated with the Cold Pool* water, and an inflow of low* | prominent role in regulating sea‐surface* pHT, driving it* | the pHT decrease caused by the anthropogenic carbon | to processes such as water masses shifting, ocean

摘要： DOM pool* rivaling the amount of carbon stored in the* | carbon cycles, transporting organic matter from | ecosystems on land to the Arctic Ocean. However, polar | releasing hundreds of tons of carbon* currently stored in* | surface waters. Dissolved organic matter (DOM) is a

摘要： organic carbon* from the ocean surface to its interior is* | exerting control over ocean-atmosphere carbon* dioxide* | , resulting in rapid turnover of the suspended carbon pool | a significant term in the global carbon* cycle* | . Most sinking organic carbon* is, however*