George T.F. Wong

ORCID: 0000-0003-4510-130X
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About
Contact & Profiles
Research Areas
  • Marine and coastal ecosystems
  • Oceanographic and Atmospheric Processes
  • Isotope Analysis in Ecology
  • Water Quality Monitoring and Analysis
  • Marine Biology and Ecology Research
  • Mercury impact and mitigation studies
  • Ocean Acidification Effects and Responses
  • Radioactive contamination and transfer
  • Marine and fisheries research
  • Coral and Marine Ecosystems Studies
  • Geological and Geophysical Studies
  • Analytical Chemistry and Sensors
  • Groundwater and Isotope Geochemistry
  • Methane Hydrates and Related Phenomena
  • Heavy metals in environment
  • Radioactive element chemistry and processing
  • Atmospheric chemistry and aerosols
  • Geology and Paleoclimatology Research
  • Microbial Community Ecology and Physiology
  • Marine Bivalve and Aquaculture Studies
  • Advanced Chemical Sensor Technologies
  • Coastal and Marine Management
  • Selenium in Biological Systems
  • Radioactivity and Radon Measurements
  • Water Treatment and Disinfection

Old Dominion University
2002-2020

Research Center for Environmental Changes, Academia Sinica
2009-2020

National Central University
2010-2015

University of Malaya
2015

Academia Sinica
2008-2014

National Science and Technology Council
2000

University of Indianapolis
1990

Indiana University – Purdue University Indianapolis
1990

National Taiwan Ocean University
1990

National Taiwan University
1990

New evidence based on recent satellite data is presented to provide a rare opportunity in quantifying the long‐speculated contribution of tropical cyclones enhance ocean primary production. In July 2000, moderate cyclone Kai‐Tak passed over South China Sea (SCS). During its short 3‐day stay, triggered an average 30‐fold increase surface chlorophyll‐a concentration. The estimated carbon fixation resulting from this event alone 0.8 Mt, or 2–4% SCS's annual new Given 14 passing SCS annually, we...

10.1029/2003gl017141 article EN Geophysical Research Letters 2003-07-01

A distinctive seasonal pattern in phytoplankton biomass was observed at the South East Asian Time‐series Study (SEATS) station (18°N, 116°E) northern China Sea (SCS). Surface chlorophyll‐ a , depth‐integrated and primary production were elevated to 0.3 mg/m 3 ∼35 2 300 mg‐C/m /d, respectively, winter but stayed low, ≤0.1 ∼15 110 /d as commonly found other low latitude waters, rest of year. Concomitantly, soluble reactive phosphate nitrate+nitrite mixed layer also became readily detectable...

10.1029/2004gl022111 article EN Geophysical Research Letters 2005-04-01

The atmospheric flux of 7 Be over a 2‐year period at coastal site (Norfolk, Virginia) and an inland (Oak Ridge, Tennessee) typically supports inventories ranging from 1.0 to 2.0 pCi/cm 2 (1 pCi = 0.037 Bq), with the highest generally occurring in spring lowest fall. calculated average daily fluxes required support these range 0.013 0.026 cm −2 d −1 . Despite different production‐source terms for 210 Pb, there is high degree correlation between their measured total monthly deposition...

10.1029/jd090id06p10487 article EN Journal of Geophysical Research Atmospheres 1985-10-20

10.1016/0012-821x(76)90084-4 article EN Earth and Planetary Science Letters 1976-10-01

10.1016/0016-7037(77)90195-8 article EN Geochimica et Cosmochimica Acta 1977-01-01

10.1016/0012-821x(75)90179-x article EN Earth and Planetary Science Letters 1975-05-01

With the rapid rise in pollution-associated nitrogen inputs to western Pacific, it has been suggested that even open ocean affected. In a coral core from Dongsha Atoll, remote reef ecosystem, we observe decline 15N/14N of skeleton-bound organic matter, which signals increased deposition anthropogenic atmospheric N on and its incorporation into plankton and, turn, atoll corals. The first clear change occurred just before 2000 CE, decades later than predicted by other work. amplitude suggests...

10.1126/science.aal3869 article EN Science 2017-05-18

Abstract A 2 °C increase in global temperature above pre-industrial levels is considered a reasonable target for avoiding the most devastating impacts of anthropogenic climate change. In June 2015, sea surface (SST) South China Sea (SCS) increased by response to developing Pacific El Niño. On its own, this moderate, short-lived warming was unlikely cause widespread damage coral reefs region, and reef “Bleaching Alert” alarm not raised. However, on Dongsha Atoll, northern SCS, unusually weak...

10.1038/srep44586 article EN cc-by Scientific Reports 2017-03-23

Abstract Coral reefs are built of calcium carbonate (CaCO 3 ) produced biogenically by a diversity calcifying plants, animals, and microbes. As the ocean warms acidifies, there is mounting concern that declining calcification rates could shift coral reef CaCO budgets from net accretion to dissolution. We quantified ecosystem (NEC) production (NEP) on Dongsha Atoll, northern South China Sea, over 2 week period included transient bleaching event. Peak daytime pH wide, shallow flat during...

10.1002/2016jc012326 article EN publisher-specific-oa Journal of Geophysical Research Oceans 2017-01-01

Abstract Internal waves can influence water properties in coastal ecosystems through the shoreward transport and mixing of subthermocline into nearshore region. In June 2014, a field experiment was conducted at Dongsha Atoll northern South China Sea to study impact internal on coral reef. Instrumentation included distributed temperature sensing system, which resolved spatially temporally continuous measurements over 4‐km cross‐reef section from lagoon 50‐m depth fore Our observations show...

10.1002/lno.11162 article EN cc-by Limnology and Oceanography 2019-03-26

10.1006/ecss.1997.0287 article EN Estuarine Coastal and Shelf Science 1998-03-01

Atmospheric depositional fluxes of 7 Be and 210 Pb were measured simultaneously in wet‐only bulk deposition over a 29‐month period (October 1982 through February 1985) Norfolk, Virginia (36°53′N, 76°18′W). Total precipitation accumulation during 1983 1984 was 134 129 cm, respectively, slightly above the normal yearly accumulation. The volume‐weighted average concentrations for 90 100 dpm/L, while those 5.9 6.6 respectively. annual 12.0 12.9 dpm/cm 2 (for Be) 0.79 0.85 Pb), There high degree...

10.1029/jd094id08p11106 article EN Journal of Geophysical Research Atmospheres 1989-08-20

10.1016/j.dsr2.2007.05.011 article EN Deep Sea Research Part II Topical Studies in Oceanography 2007-07-01

volcanic particles and a phytoplankton bloom. FLH was found to be ∼9–17 × 10 −3 mW cm −2 mm −1 sr in the patch ∼3– 5×1 0 ambient water, indicating that 2–5‐fold increase biological activity occurred during week following eruption. Satellite altimetry indicated bloom took place presence of downwelling not result upwelled nutrients this oligotrophic ocean. Analysis satellite ocean color spectra region similar as reference Trichodesmium spectra. Laboratory experiments further substantiate...

10.1029/2009gb003758 article EN Global Biogeochemical Cycles 2011-02-25

Significance Biologically available nitrogen (fixed N) limits the fertility of much ocean. Of processes that remove fixed N from ocean, conversion to 2 in coastal sediments appears dominate. This work provides strongest data-based support for long-standing hypothesis changes loss along ocean margin due cyclic drowning and emergence continental shelves. The data also imply strong local coupling fixation, dominant input thus suggesting a stable oceanic reservoir over glacial cycles. Finally,...

10.1073/pnas.1701315114 article EN Proceedings of the National Academy of Sciences 2017-07-31

10.1016/0043-1354(77)90154-3 article EN Water Research 1977-01-01
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