Chao Zhang

ORCID: 0000-0003-0320-2356
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About
Contact & Profiles
Research Areas
  • Atmospheric chemistry and aerosols
  • Air Quality and Health Impacts
  • Atmospheric Ozone and Climate
  • Atmospheric aerosols and clouds
  • Cryospheric studies and observations
  • Atmospheric and Environmental Gas Dynamics
  • nanoparticles nucleation surface interactions
  • Marine Biology and Ecology Research
  • Marine and coastal ecosystems
  • Oceanographic and Atmospheric Processes
  • Subterranean biodiversity and taxonomy
  • Arctic and Antarctic ice dynamics
  • Air Quality Monitoring and Forecasting
  • Climate variability and models
  • Per- and polyfluoroalkyl substances research
  • Heavy metals in environment
  • Environmental DNA in Biodiversity Studies
  • Geophysics and Gravity Measurements
  • Fluid Dynamics and Heat Transfer
  • Methane Hydrates and Related Phenomena
  • Aeolian processes and effects
  • Hydrocarbon exploration and reservoir analysis
  • Animal Diversity and Health Studies
  • Marine and fisheries research
  • Aquatic and Environmental Studies

Xiamen University
2023-2025

Chinese Academy of Sciences
2019-2024

University of Chinese Academy of Sciences
2020-2024

Northwest Institute of Eco-Environment and Resources
2023-2024

Institute of Tibetan Plateau Research
2020-2023

Southwest University
2023

University of Shanghai for Science and Technology
2021-2023

Qingdao National Laboratory for Marine Science and Technology
2023

Ocean University of China
2020-2023

China Meteorological Administration
2023

Abstract Carbon dioxide (CO 2 ) and methane (CH 4 emissions from freshwater ecosystems are predicted to increase under climate warming. However, in glacierized regions differ critically those non-glacierized regions. The potential of CO CH environments the Tibetan Plateau (TP) were only recently recognized. Here, first direct measurement emission fluxes isotopic composition during spring 2022 13 glacial lakes TP revealed that previously overlooked sinks due chemical weathering daily average...

10.1088/1748-9326/aceb7b article EN cc-by Environmental Research Letters 2023-07-28

The surface air temperature (SAT) over the Tibetan Plateau (TP) not only affects physical processes such as local evaporation, snow melting, and glacier ablation, but also has a great impact on downstream regions even global climate change. development of reanalysis data gradually overcome problem sparse stations TP, there are still some deficiencies. Therefore, distance between indices simulation observation (DISO) method is used to calculate five datasets (ERA5, JRA-55, ERA-Interim,...

10.3389/fenvs.2023.1152129 article EN cc-by Frontiers in Environmental Science 2023-03-07

Climatic fingerprint of Heinrich (H) events was characterized by widespread megadroughts over the Asian summer monsoon (ASM) region accompanied systemic weakening ASM. However, recent studies hydroclimate proxies suggest huge spatial discrepancies in precipitation ASM during some H events, increased Yangtze River Valley contrasting with prevalent across whole region. The mechanism responsible for and relationship between local intensity remain elusive. In this study, we investigate response...

10.5194/egusphere-egu25-8041 preprint EN 2025-03-14

Abstract. Water-soluble inorganic ions such as ammonium, nitrate and sulfate are major components of fine aerosols in the atmosphere widely used estimation aerosol acidity. However, different experimental practices instrumentation may lead to uncertainties ion concentrations. Here, an intercomparison experiment was conducted 10 laboratories (labs) investigate consistency concentrations resultant acidity estimates using same set filter samples. The results mostly exhibited good agreement for...

10.5194/amt-13-6325-2020 article EN cc-by Atmospheric measurement techniques 2020-11-25

Abstract We present a new, biostratigraphically calibrated organic and inorganic C-isotope record spanning the basal Late Permian to earliest Triassic from southern Guizhou (Nanpanjiang basin, South China). After fluctuations of likely diagenetic overprint are removed, three negative carbon isotope excursions (CIEs) persist. These include short-lived CIE during early Wuchiapingian, protracted ending shortly after Wuchiapingian–Changhsingian Boundary, third straddling Permian–Triassic...

10.1130/b31996.1 article EN Geological Society of America Bulletin 2019-07-16

Carbonaceous aerosols play an important role in radiative forcing the remote and climate-sensitive Tibetan Plateau (TP). However, sources of carbonaceous to TP remain poorly defined, part due lack regionally relevant data about aerosols. To address this knowledge gap, we present first comprehensive analysis δ13C signatures aerosol endmembers local TP, encompassing total carbon, water-insoluble particle elemental carbon originating from fossil fuel combustion, biomass topsoil. The these...

10.1021/acs.est.3c09357 article EN Environmental Science & Technology 2024-05-23

The genus Plistobunus Pocock, 1903 and its type species rapax are redescribed based on the material deposited in British Museum of Natural History (BMNH), London. In addition, a new from Hainan Island is described illustrated columnariussp. n. diagnosed by having row 12 setiferous tubercles anterior margin carapace, femur pedipalpus ventrally with 13 male.

10.3897/zookeys.112.1110 article EN cc-by ZooKeys 2011-06-24
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