Sentences with phrase «understood atmospheric water»
People that don't know why there are water towers are supposed to understand atmospheric water vapor, CO3 (as in CaCO3!
https://dotearth.blogs.nytimes.com/ Not exact matches
One topic of interest is reactions involving water and CO2, to aid understanding of how atmospheric CO2 interacts with and acidifies the oceans.
The objective of the MAVEN mission EPO program is to engage multiple audiences in the quest to understand Mars» long - term atmospheric losses, giving insight into the history of Mars» atmosphere and climate, liquid water, and planetary habitability.
The objective of the MAVEN mission E / PO program is to engage multiple audiences in the quest to understand Mars» long - term atmospheric losses, giving insight into the history of Mars» atmosphere and climate, liquid water, and planetary habitability.
Cornerstone Evaluation Associates LLC is the external research firm charged with carrying out the evaluation activities necessary to determine the effectiveness and impact of MAVEN's Education and Public Outreach (E / PO) effort and its success in achieving its overall goal to «engage multiple audiences in the quest to understand Mars» long - term atmospheric losses, giving insight into the history of Mars» atmosphere and climate, liquid water, and planetary habitability.»
His current research is mainly focused on the application of efficient computational methods to understand the structure and dynamics of hydrogen - bonded systems ranging from water clusters to atmospheric aerosols.
It is now widely recognized that improvements in understanding and predicting climate hinge largely on a better understanding of the processes controlling atmospheric water vapor.»
For new technologies the ETA team often starts with a life - cycle energy, water, or materials analysis to understand the technology's impacts when scaled up, and then uses other models as needed, such as an atmospheric chemistry model or energy system model.
«Trends in observed atmospheric water vapour are hampered by inhomogeneities in data records, which occur when measurement programmes are discontinued because of, for example, the limited lifespans of satellite missions or insufficiently documented or understood changes in instrumentation.
The future monitoring of atmospheric processes involving water vapor will be critical to fully understand the feedbacks in the climate system leading to global climate change.
It's my understanding that NVAP data shows as atmospheric CO2 increases, water vapor decreases; exactly opposite what climate models predict because they assume water vapor is a net positive feedback; more wv, more warming, more wv, more warming.....
With your water pot analogy, I don't understand how heating from below the water is equivalent to atmospheric warming.
In that regard, atmospheric and terrestrial processes and their long - term interactions need to be understood to better support policies on water management.
Motivated by findings that major components of so - called cloud «feedbacks» are best understood as rapid responses to CO2 forcing (Gregory and Webb in J Clim 21:58 — 71, 2008), the top of atmosphere (TOA) radiative effects from forcing, and the subsequent responses to global surface temperature changes from all «atmospheric feedbacks» (water vapour, lapse rate, surface albedo, «surface temperature» and cloud) are examined in detail in a General Circulation Model.
Thus an understanding of the mechanisms distributing water vapor through the atmosphere and of water vapor's effects on atmospheric radiation and circulation is vital to estimating long - term changes in climate.
Based on the understanding of both the physical processes that control key climate feedbacks (see Section 8.6.3), and also the origin of inter-model differences in the simulation of feedbacks (see Section 8.6.2), the following climate characteristics appear to be particularly important: (i) for the water vapour and lapse rate feedbacks, the response of upper - tropospheric RH and lapse rate to interannual or decadal changes in climate; (ii) for cloud feedbacks, the response of boundary - layer clouds and anvil clouds to a change in surface or atmospheric conditions and the change in cloud radiative properties associated with a change in extratropical synoptic weather systems; (iii) for snow albedo feedbacks, the relationship between surface air temperature and snow melt over northern land areas during spring and (iv) for sea ice feedbacks, the simulation of sea ice thickness.
CO; 2 Observations of the Infrared Radiative Properties of the Ocean «[I] t is necessary to understand the physical variables contributing to sea surface emitted and reflected radiation to space.The emissivity of the ocean surface varies with view angle and sea state, the reflection of sky radiation also depends on view angle and sea state, and the absorption of atmospheric constituents such as water vapor, aerosols, and subdivisible clouds affect transmittance.»
Scientists measured properties of water at deeply supercooled temperatures — which may help theorists flesh out their understanding of water and help atmospheric scientists better understand rain and clouds.
Similarly, UCSB researchers (results to be published in the journal Physical Review Letters) «filled the laboratory cylinders with water, and heated the water from below and cooled it from above,» to better understand the dynamics of atmospheric circulation and «swirling natural phenomena» observed in nature.