Not exact matches
«While
transporting Breivik to prison
via an aircraft, the cabin door suddenly opened and he fell 30,000 ft.. He did not survive the frigid
waters of the North Atlantic.»
In the early study draft, author Paul Heisig noted that gas «drilling, extraction,
transport via pipelines, and underground storage» could inadvertently introduce methane into drinking
water supplies.
«In the early study draft, author Paul Heisig noted that gas «drilling, extraction,
transport via pipelines, and underground storage» could inadvertently introduce methane into drinking
water supplies,» Capital New York's Scott Waldman wrote.
This can occur if field or laboratory equipment is contaminated or if DNA is
transported long distances
via predators or
water currents.
Cold, polar
waters constantly absorb CO2, sink as it becomes more dense, and is
transported to the equatorial
waters via the ThermoHaline and outgases in the warmer
waters of the Indian and Pacific Oceans.
Dan H.: «Cold, polar
waters constantly absorb CO2, sink as it becomes more dense, and is
transported to the equatorial
waters via the ThermoHaline and outgases in the warmer
waters of the Indian and Pacific Oceans.»
The surface
waters of the tropical Atlantic are then
transported,
via the Gulf Stream, towards the high latitudes where they warm the atmosphere before plunging into the abysses in the convection zones situated in the seas of Norway, Greenland and Labrador.
Thus it appears that disruption of deep
water formation in the North Atlantic,
via a blob of colder fresher
water coming off of Greenland, would not «shut down» or even affect the Gulf Stream net mass
transport at all, but instead would shift its northern return flow southwards, with many severe regional consequences.
Warm surface
water flows from the tropical South Atlantic, through the Caribbean, and is then
transported,
via the Gulf Stream and North Atlantic Drift, to the northernmost North Atlantic.
Storms help replenish warm
water next to the ice, and help carry addtional heat into the melting region
via atmospheric
transport of warmer moist air.
Atmospheric
water vapor and cloud distributions are the direct results of the model physics interactions (
via evaporation,
transport, condensation, precipitation).
Next year, I expect sea ice free conditions in the Arctic based on heat
transport via water vapor in the Arctic atmosphere, storm conditions driven by latent heat in the atmosphere, and a good deal of snow this fall that insulates sea ice and permafrost from the cold, thereby allowing them to remain warm and weak.
This is usually accompanied by an impaired ability to
transport water to the leaves
via the outer xylem (the sapwood), courtesy of blue stain fungi (e.g. Grosmannia or Ceratocystis spp.) carried and introduced by the beetles.
Topics that I work on or plan to work in the future include studies of: + missing aerosol species and sources, such as the primary oceanic aerosols and their importance on the remote marine atmosphere, the in - cloud and aerosol
water aqueous formation of organic aerosols that can lead to brown carbon formation, the primary terrestrial biological particles, and the organic nitrogen + missing aerosol parameterizations, such as the effect of aerosol mixing on cloud condensation nuclei and aerosol absorption, the semi-volatility of primary organic aerosols, the importance of in - canopy processes on natural terrestrial aerosol and aerosol precursor sources, and the mineral dust iron solubility and bioavailability + the change of aerosol burden and its spatiotemporal distribution, especially with regard to its role and importance on gas - phase chemistry
via photolysis rates changes and heterogeneous reactions in the atmosphere, as well as their effect on key gas - phase species like ozone + the physical and optical properties of aerosols, which affect aerosol
transport, lifetime, and light scattering and absorption, with the latter being very sensitive to the vertical distribution of absorbing aerosols + aerosol - cloud interactions, which include cloud activation, the aerosol indirect effect and the impact of clouds on aerosol removal + changes on climate and feedbacks related with all these topics In order to understand the climate system as a whole, improve the aerosol representation in the GISS ModelE2 and contribute to future IPCC climate change assessments and CMIP activities, I am also interested in understanding the importance of natural and anthropogenic aerosol changes in the atmosphere on the terrestrial biosphere, the ocean and climate.