Results 171 to 180 of about 10,025 (269)
Methane Emissions Offsetting With Temporary Carbon Sinks
A time‐explicit framework based on atmospheric impulse–response functions quantifies the CO2 removal required to offset methane warming within 20 years. Constant, variable, and increasing carbon sinks each demand different removal masses, demonstrating that sink timing—not just permanence—determines the climate value of temporary carbon storage ...
Hans‐Peter Schmidt, Nikolas Hagemann
wiley +1 more source
Ocean Carbon Dioxide Removal and Storage. [PDF]
Lee CH, Subhas AV, Kim JH, Lee K.
europepmc +1 more source
ABSTRACT As breath‐hold divers, marine mammals must coordinate their use of both aerobic and anaerobic metabolism to maximize their time at depth. One indication of the relative reliance between these two energy‐producing systems is the aerobic dive limit (ADL), defined as the dive duration where post‐dive blood lactate concentrations surpass resting ...
Aaron S. Purdy, David A. S. Rosen
wiley +1 more source
Abstract Southern Hemisphere westerly winds are important drivers of Antarctic and sub‐Antarctic environmental change. Short observational wind records prevent us from fully understanding the scope of their variability. Proxy records provide valuable tools to extend environmental records. Here we present a novel wind study based on the use of windblown
Dieter R. Tetzner +4 more
wiley +1 more source
Tubular Membrane Coupled with Marine Waste-Derived Hybrid Adsorbent for Textile Micropollutant Removal and Photochemical Regeneration. [PDF]
Chihi R +4 more
europepmc +1 more source
Anthropogenic Carbon Isotope Signals in North Atlantic Water Masses at 48°N
Abstract Deep‐water masses are formed in the North‐Atlantic, making studies of δ13C of dissolved CO2 in this region key to monitor and understand the spreading of anthropogenic carbon into the ocean interior. The objective of this study is to quantify the Suess effect (SE) in North Atlantic water masses using sulfur hexafluoride (SF6) as the ...
E. Bavoux +5 more
wiley +1 more source
Maximum Lifetime of the Vegetative Biosphere
Abstract We use a three‐dimensional model to calculate steady‐state climates at various intervals in Earth's future, across a parameter space of increasing insolation and decreasing CO2 ${\text{CO}}_{2}$ mixing ratio. Comparison with prior results shows an overestimation of warming by one‐dimensional models when solar constant is increased and CO2 ...
Jacob Haqq‐Misra, Eric Wolf
wiley +1 more source
Can microalgae grow on dissolved black carbon generated from high-frequency wildfires? [PDF]
Faisal S +14 more
europepmc +1 more source
Abstract Anthropogenic aerosol effective radiative forcing (ERF) remains one of the largest uncertainties in quantifying the human influence on climate. Estimates of aerosol ERF depend on the background meteorological state and composition, including factors such as cloud regimes, circulation, and pre‐existing aerosol and precursor levels.
Shipeng Zhang +3 more
wiley +1 more source
Characterization of phytoplankton-excreted metabolites mediating carbon flux through the surface ocean. [PDF]
Zhu Y +10 more
europepmc +1 more source

