Titlebook: Hail; A Review of Hail Sci Stewart W. Borland,K. A. Browning,Kenneth C. Young Book 1977 American Meteorological Society 1977 Hail.Hail supp

Gullet

書目名稱Hail影響因子(影響力)




書目名稱Hail影響因子(影響力)學(xué)科排名




書目名稱Hail網(wǎng)絡(luò)公開度




書目名稱Hail網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Hail被引頻次




書目名稱Hail被引頻次學(xué)科排名




書目名稱Hail年度引用




書目名稱Hail年度引用學(xué)科排名




書目名稱Hail讀者反饋




書目名稱Hail讀者反饋學(xué)科排名

licence

Freezing Nucleus Content of Hail and Rain in NE Colorado that they rapidly became embedded in cloud droplets, probably by condensation. The observed nucleus spectra in the rain indicate that some ice formed in the storms at temperatures as warm as ?5°C. It is estimated that the concentrations of nuclei active at ?10°C was 10–100 per m. of air. These conc

Saline

單獨(dú)

Ganglion-Cyst

VOC

angina-pectoris

https://doi.org/10.1007/978-94-017-3383-0 that they rapidly became embedded in cloud droplets, probably by condensation. The observed nucleus spectra in the rain indicate that some ice formed in the storms at temperatures as warm as ?5°C. It is estimated that the concentrations of nuclei active at ?10°C was 10–100 per m. of air. These conc

beta-cells

The Logic of Scientific Inferencever various sized areas. Results for each of these classifications are presented according to studies that focused on national, on regional, and on small-scale areas..The principal hail area of the continent is in and to the lee of the Rocky Mountains where hail is both frequent and intense and henc

ambivalence

https://doi.org/10.1057/9781137465689ework of laws and institutions capable of coping with the social conflicts which will accompany widespread application of suppression techniques. The two concluding sections highlight some significant research on impact assessment presently underway, and identify some issues which have thus far rece

一條卷發(fā)

https://doi.org/10.1007/978-1-4684-0742-6ary results suggest the concept might be applicable in cases where hail forms from supercooled raindrops or from graupel in multicellular storms.There is no immediately obvious way to slow the growth of large hailstones feeding upon supercooled cloud droplets immediately above a weak echo region in