Measuring and
modeling carbon dioxide and water vapor exchange over a temperate broad - leaved forest during the 1995 summer drought
Not exact matches
Interior Astronomers hoped the probe would confirm that comets fit the popular
model of a «dirty snowball»: an icy core made up of a solid mix of
water ice, dirt,
and frozen gases like
carbon dioxide and carbon monoxide, coated with a thin crust of debris.
Like older
models, they will use uranium fission to heat
water and drive a turbine, but these reactors will be smaller, simpler to build,
and each will add more than 1100 megawatts of capacity to the region's power grid when they come online in 2016 or 2017 — without emitting
carbon dioxide.
To improve
models for drilling, hydraulic fracturing
and underground storage of
carbon dioxide, Oak Ridge National Laboratory scientists used neutrons to understand how
water flows through fractured rock.
The short -
and long - wave absorptivities of the most important greenhouse gases
water vapour,
carbon dioxide, methane
and ozone are derived from line - by - line calculations based on the HITRAN08 - databasis
and are integrated in the
model.
Data from satellite observations «suggest that greenhouse
models ignore negative feedback produced by clouds
and by
water vapor, that diminish the warming effects» of human
carbon dioxide emissions.
The short -
and long - wave absorptivities of the most important greenhouse gases
water vapour,
carbon dioxide, methane
and ozone are derived from line - by - line calculations based on the HITRAN08 - databasis
and are integrated in the
model.
Climate
models also indicate that greenhouse gases such as
carbon dioxide and methane may enhance the transport of
water into the stratosphere»
Model simulations indicate that polar surface
waters will become undersaturated for aragonite in the near future for the Arctic (atmospheric
carbon dioxide of 400 - 450 ppm)
and by mid-century for the southern ocean off the Antarctic (atmospheric
carbon dioxide of 550 - 600 ppm).
These
models suggest that if the net effect of ocean circulation,
water vapour, cloud,
and snow feedbacks were zero, the approximate temperature response to a doubling of
carbon dioxide from pre-industrial levels would be a 1oC warming.
To name two examples, both John Tyndall — who first discovered the roles of
water vapor
and carbon dioxide as greenhouse gases in 1859 - 60 —
and Svante Arrhenius — who hand - calculated the first
model of greenhouse warming in 1896 — used this terminology in the titles of their ground - breaking papers.
They do so because within these
models the far more important radiative substances,
water vapor
and clouds, act to greatly amplify whatever an increase in
carbon dioxide might do.
Indeed, strong observational evidence
and results from
modeling studies indicate that, at least over the last 50 years, human activities are a major contributor to climate change.Direct human impact is through changes in the concentration of certain trace gases such as
carbon dioxide, chlorofluorocarbons, methane, nitrous oxide, ozone,
and water vapor, known collectively as greenhouse gases.
The world's climate is way too complex... with way too many significant global
and regional variables (e.g., solar, volcanic
and geologic activity, variations in the strength
and path of the jet stream
and major ocean currents, the seasons created by the tilt of the earth,
and the concentration of
water vapor in the atmosphere, which by the way is many times more effective at holding heat near the surface of the earth than is
carbon dioxide, a non-toxic, trace gas that all plant life must have to survive,
and that produce the oxygen that WE need to survive) to consider for any so - called climate
model to generate a reliable
and reproducible predictive
model.
Climate
models focus on the effect of greenhouse gases, primarily
carbon dioxide and water vapor, to the neglect of cloud cover.
Current global climate
models suggest that the
water vapor feedback to global warming due to
carbon dioxide increases is weak but these
models do not fully resolve the tropopause or the cold point, nor do they completely represent the QBO [Quasi Biennial Oscillation], deep convective transport
and its linkages to SSTs, or the impact of aerosol heating on
water input to the stratosphere.
Specific research topics include
carbon dioxide, methane
and water fluxes
and their reservoirs in vegetation
and soil, transport in atmosphere,
and model - data fusion using advanced numerical methods.The research is based on numerical
modelling, from local to global scale with focus on northern regions.
Satellite observations suggest that GH
models ignore negative feedbacks, produced by clouds
and by
water vapor, that diminish the warming effects of
carbon dioxide.»
Bear in mind that the representation of clouds in climate
models (
and of the
water vapour which is intimately involved with cloud formation) is such as to amplify the forecast global warming from increasing atmospheric
carbon dioxide — on average over most of the
models — by a factor of about three (5).
Climate
models encapsulate what we know about how the Sun's rays travel through the atmosphere
and how heat from the surface of the Earth gets absorbed by clouds,
water vapour
and, of course,
carbon dioxide.