Results 221 to 230 of about 84,293 (267)

An observational case study for inorganic nitrogen dry deposition potential on sea-surface primary production in the subtropical, western North Pacific. [PDF]

Sci Rep
Taketani F, Matsumoto K, Sekiya T, Yamaji K, Kanaya Y.   +4 more
europepmc   +1 more source

Historical deforestation drives strong rainfall decline across the southern Amazon basin. [PDF]

Nat Commun
Cui J, Piao S, Huntingford C, Wang T, Spracklen DV.   +4 more
europepmc   +1 more source

Standardized radar wind profiler dataset via integrated raw data processing in Korea. [PDF]

Sci Data
Lee K, Kwon BH, Lee J, Yoon S, Kwon S, Jung SH.   +5 more
europepmc   +1 more source

Preflight Calibration and Performance Assessment of the Geostationary Interferometric Infrared Sounder (GIIRS) Onboard the FengYun-4B Satellite. [PDF]

Sensors (Basel)
Lee L, Li L, Zou Y, Wang Z, Han C, Zhang L, Ding L.   +6 more
europepmc   +1 more source

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Atmospheric processes and observations

Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 2003
The central role of the atmosphere in abrupt climate change is proposed and discussed. This discussion is given in the context of the poleward transport of energy in the climate system and of climate variability and change. A number of examples based on observational and model data are used to illustrate the ideas.
openaire   +2 more sources

Atmospheric glories: simulations and observations

Applied Optics, 2005
Mie theory can be used to provide full-color simulations of atmospheric glories. Comparison of such simulations with images of real glories suggests that most glories are caused by spherical water droplets with radii between 4 and 25 microm. This paper also examines the appearance of glories taking into account the size of the droplets and the width of
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Observing the Atmosphere

2003
The aim of this chapter is to give an overview of the techniques used to observe the atmosphere, and the physical principles involved. In particular, we attempt to highlight characteristics of different observation types that need to be taken into account when using them in an atmospheric data assimilation system.
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Observations by Atmospheric Radar

2013
Atmospheric radars are capable of continuously monitoring echo power spectrum in the vicinity of the zenith. From the spectrum, echo intensity, Doppler velocity, and velocity spectrum width are derivable over the wide altitude range 1–100 km in the Earth’s atmosphere. In this chapter, observations by atmospheric radar are discussed.
Shoichiro Fukao, Kyosuke Hamazu
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Atmospheric Changes and Observations

2019
Earth’s atmosphere is usually air layer of the solid Earth outer, which is an important part of the Earth’s natural environment. It is the condition indispensable to the survival of life on Earth and also protective for life on Earth. With developments and advances in space technologies, human activities are involving into the upper atmosphere and ...
Shuanggen Jin, R. Jin, X. Liu
openaire   +1 more source