Like Facebook postings or tweets that get shared over and over again, temperature and humidity get transported from one place to
another by atmospheric flows, such as winds.
Not exact matches
A mighty
atmospheric river, fueled
by water vapor from the Amazon and heat from the sun,
flows across South America until it reaches the Andes and condenses into rain.
Dr Joshi said: «The new treatment system is made
by converting naturally occurring graphite into graphene oxide membranes that allow high water
flow at
atmospheric pressure, while removing virtually all of the organic matter.»
Atmospheric science professors Nate Brunsell and David Mechem in KU's Department of Geography are co-authors of a new study just published in the Proceedings of the National Academy of Sciences
by an international research group that evaluated the effects of large wind farms on
atmospheric flow and its implications for how much renewable energy the turbines can generate.
A study published this year
by Bradley Udall, senior water and climate research scientist with the Colorado Water Institute at Colorado State University, and Jonathan Overpeck, professor of hydrology and
atmospheric sciences at the University of Arizona, found that during the drought years of 2000 - 2014, the river surrendered a third of its
flow because of higher temperatures in the upper basin.
A NOAA website on
atmospheric rivers contains this fascinating statistic that illustrates just how much moisture can be transported
by winds in the mid-to-upper atmosphere: «A strong
atmospheric river transports an amount of water vapor roughly equivalent to 7.5 - 15 times the average
flow of liquid water at the mouth of the Mississippi River.»
Jupiter's colorful
atmospheric patterns
flow alternately east and west, at speeds that differ
by up to 100 meters per second.
The
atmospheric zonal
flows extend downwards
by more than 2,000 kilometres, but not beyond 3,500 kilometres, as is also the case with the jets.
Loose enough to be
atmospheric, yet containing just enough detail to be both accurate and satisfying on closer more detailed inspection, his intuitive use of colour in bold
flowing washes, is underpinned
by his firm grasp of perspective and draftsmanship, complemented
by a strong sense of place.
Once stirred into motion, the coldest sink current in the world, dormant for 10,000 years, will transform the map of oceanic and
atmospheric current
flows, thereby making the necessary rebalances
by whatever [unknown] means necessary to maintain the second law of thermodynamics
by absolute right!
The 2 Gton / yr net CO2 invasion into the ocean is driven
by the rising
atmospheric concentration, not
by water
flow or heat fluxes or anything like that.
Thus, if the absorption of the infrared emission from
atmospheric greenhouse gases reduces the gradient through the skin layer, the
flow of heat from the ocean beneath will be reduced, leaving more of the heat introduced into the bulk of the upper oceanic layer
by the absorption of sunlight to remain there to increase water temperature.
Conversely, due to well - researched upper -
atmospheric flow (e.g. vertical shear) configurations favorable to Atlantic hurricane development and intensification, La Nina falls tend to favor very active seasons in the Atlantic (El Nino years are the converse, with must less activity, as forecast
by Gray and NOAA for 2009).
Its average
atmospheric lifetime is about 9 days, which is way too short for getting mixed properly
by turbulent
flows.
Since coming to PNNL, he has led or been significantly involved in studies of effects of surface heterogeneity on boundary layer structure, of mesoscale
atmospheric flows induced or modulated
by complex terrain, of the simulation of dust emission
by wind erosion, and of the capabilities of a variety of
atmospheric instruments — including a mass spectrometer and wind profiling radar — for measuring
atmospheric turbulence.
All
atmospheric scientists know that clouds are controlled
by a multitude of factors; my position is that causation between clouds and temperature
flows in bot directions.
The regions of large precipitation are determined
by the
atmospheric circulation: the near - surface
atmospheric flow converges near the subsolar point, leading to strong ascending motion and condensation (see Merlis and Schneider (2010) for a detailed discussion).
In cold or snow - dominated river basins,
atmospheric temperature increases do not only affect freshwater ecosystems via the warming of water (see Chapter 4) but also
by causing water -
flow alterations.
The atmosphere is analogous to a flexible lens that is shaped
by the density distribution of the gas molecules, of the atmosphere in the space between the sphere holding them, and space; Incoming heat gets collected in many ways and places,, primarily
by intermittent solar radiation gets stored, in vast quantities, and slowly but also a barrage of mass and energy fluxes from all directions; that are slowly transported great distances and to higher altitudes mostly
by oceanic and
atmospheric mass
flows.
Dynamical effects arising from changes in
atmospheric pressure also play a role in distributing meltwater, as do geostrophic ocean currents that
flow along the lines where pressure gradients are counterbalanced
by the Coriolis effect associated with the Earth's rotation.
Your claim proven as a theorem now means basically (with some radiative cooling at the top for the return
flow) that it does not need confirmation
by numerical modelling, but rather, application, to see how it plays out in real
atmospheric problems.
A detailed and very accurate calculation of the
atmospheric flows of moist air must take into account also the effects related to the volume taken
by water vapor both when water vapor is added
by evaporation and when it's removed in condensation, but these effects are very minor corrections and not a source of anything significant.
... giant planets, Saturn has an
atmospheric circulation that is dominated
by zonal (east - west)
flow.
Both a glass greenhouse and an
atmospheric greenhouse lead to higher surface temperatures
by blocking a
flow of heat upwards, while having much less effect on the heat
flow downwards.
We found that Colorado River
flows decline
by about 4 percent per degree F increase, which is roughly the same amount as the increased
atmospheric water vapor holding capacity discussed above.
You can not have the same energy
flowing freely to the space (
atmospheric window) if you have a different amount of power absorbed
by the surface.
Stable and accurate solutions to the Navier Stokes equations for large scale
atmospheric flows are obtained
by filtering sound waves (the hydrostatic assumption) and filtering high frequency unresolved gravity waves.
Driven primarily
by atmospheric stresses, these ice bridges are formed when sufficiently thick ice «jams» during the course of its
flow between land masses, resulting in a region of stationary compacted ice that is separated from a region of
flowing open water (a polynya)
by a static arch.