It is versatile because an atomic force microscope can not only image in three - dimensional topography, but it also provides various
types of surface measurements to the needs of scientists and engineers.
Not exact matches
With
surface measurements alone, it's hard to confirm the
type - II Weyl fermions are there, says physicist Alexey Soluyanov
of ETH Zurich.
Atmospheric
measurements, from below ground It may seem incredible that atmospheric change can be measured below ground, but seismic sensors record all
types of surface movement — even delineating day from night, or weekends from weekdays when placed near cities.
While satellites have provided consistently good data for years, the next frontier in sea level rise
measurement is a new
type of radar that can capture a more crisp, higher - resolution picture
of sea
surface heights.
Physicists at the University
of Washington have conducted the most precise and controlled
measurements yet
of the interaction between the atoms and molecules that comprise air and the
type of carbon
surface used in battery electrodes and air filters — key information for improving those technologies.
In the case
of ORAS4, this includes ocean temperature
measurements from bathythermographs and the Argo buoys, and other
types of data like sea
surface height and
surface temperatures.
These algorithms, developed for national and international operational and research satellite programs, convert sensor / instrument
measurements into geophysical parameters such as vertical temperature / water vapor profiles, estimates
of cloud amount,
type and phase, and land / ocean parameters such as sea
surface winds, net heat flux, and forest fire intensity / extent.
Pekka, the approximately uniform prior in Y is, according to F&G, a consequence
of a) the choice
of an OLS regression
type, b) the fact that the combined errors in the
measurements of forcings and net radiative balance were very much greater than errors in
measurements of the
surface temperature, and c) the assumption
of normal distributions in the errors
of the three observables.
My point is that in the absence
of such a fine grid, one should place the
measurement locations according to the well studied rules
of polling: Decide on the number
of types of environment: urban, desert, mountain, iceberg, tropics, etc and weight the results according to the percentage each
of these
types have on the
surface of the globe.
All temperature reconstructions suffer from one VERY arbitrary assumption in relation to the
measurement method
of sea
surface temperatures SST (buckets
of various
types, engine):
The «scientific» circus
of surface temperature
measurement based on cool canvas buckets, hot wooden outhouses, ice - covered balloons and endless ad hoc «adjustments» is ripe for a Feynman -
type send - up.
We also need in situ
measurements in the GrIS's ablation zone that can distinguish the relative contributions
of different impurity
types (e.g., black carbon, dust, algae) to albedo reduction as well as models that accurately simulate the GrIS
surface energy balance and mass balance.