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Cm-sized carbonate seafloor fans occur in the Neoproterozoic Rainstorm Member of the Johnnie Formation, Death Valley, USA. The fans formed in a mixed carbonate-clastic succession near storm wave base at the base of parasequences on a storm-dominated ramp. ... Although not directly dated, ... PDF; Restricted to Caltech users only ;
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authors.library.caltech.edu/12179/
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An animation illustrates the formation of rain storms in this vicinity. The effect of the sea breezes in the Gulf of Chihili can be seen. ... An animation illustrates the formation of rain storms in this vicinity. A convergence zone along the coast of the Gulf of Tonkin and South China Sea can be seen.
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www.research.ibm.com/weather/CMA/CMA.html
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To focus on the conditions of the formation and development of rainstorm, the thermal and dynamical characters of the mesoscale system of this Meiyu front ...
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linkinghub.elsevier.com/retrieve/pii/S1001605806601388
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During rainstorms, physical properties of the soil surface change ..... The dynamics of seal formation in subsequent storms depend mainly on the soil type ...
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linkinghub.elsevier.com/retrieve/pii/S0341816299000260
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As a process, it can move by formation and dissipation. What we see as a continuous convective storm can be the result of new cells forming on one flank of preceding cells, eventually becoming "the storm" as the older cells dissipate.
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www.cimms.ou.edu/~doswell/barcelona/Barcelona_Rain.html
www.cimms.ou.edu/~doswell/barcelona/Barcelona_Rain.html
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Rain - Wikipedia, the free encyclopedia
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Rain is liquid precipitation, as opposed to other kinds of precipitation such as snow, hail and sleet. On Earth, it is the condensation of atmospheric water vapor into drops heavy enough to fall, oft...
en.wikipedia.org/wiki/Rain
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Surprisingly little is known about the basic physics of rain formation, despite its relevance to everyday life and to weather forecasting. ... ; Turbulence whips up rainstorms...
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www.nature.com/nature/links/020912/020912-3.html
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Thus, floods in creeks and small rivers close to the river head (i.e. with a small catchment area) are characterised by faster runoff formation after heavy rainstorms and flood waves generated during or directly after the precipitation event.
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nadine.helmholtz-eos.de/risks/flood/info/fl_system_en.h...
nadine.helmholtz-eos.de/risks/flood/info/fl_system_en.html
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The rivers will not be able to contain flood flow within its banks during heavy rainstorms. The existing drainage conditions are summarized in Table 2.1. ... The formation of flood plain flow area requires substantial land resumption.
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www.epd.gov.hk/eia/register/report/eiareport/eia_110200...
www.epd.gov.hk/eia/register/report/eiareport/eia_1102005/eia_report/HTML/Sec%202.htm
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