'Mean wind' presentation slideshows

Dr. Sam C M Hui Department of Mechanical Engineering The University of Hong Kong E-mail: cmhui@hku.hk

663 views • 46 slides

Lackmann , Chapter 1:

Lackmann , Chapter 1:. Basics of atmospheric motion. time scales of atmospheric variability. Lovejoy 2013, EOS . time scales of atmospheric variability. Lovejoy 2013, EOS . (1) Scales of atmospheric motion. Note two spectral extremes: (a) A maximum at about 2000 km

518 views • 37 slides

Chapter 9

489 views • 35 slides

TEKNIK PENGUKURAN POTENSI ENERGI ANGIN

TEKNIK PENGUKURAN POTENSI ENERGI ANGIN. Bidang Konversi Energi Dirgantara LAPAN. Malik Ibrochim. WIND CAUSED. Wind is caused by differences in pressure. When a difference in pressure exists, the air is accelerated from higher to lower pressure

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5.3 What control occurrence, intensity, type and life-time of the convective systems?

5.3 What control occurrence, intensity, type and life-time of the convective systems?. Central questions What control the occurrence of convection? What control convective type (intensity, lift time, dynamic structure)?. What control occurrence of convection?. Question:

196 views • 8 slides

The problem: bias in filtered & unfiltered KE (contours) and mean wind (vectors)

The problem: bias in filtered & unfiltered KE (contours) and mean wind (vectors). Unfiltered (KE). Filtered (EKE). Excessively zonal mean wind extending into E urope, made worse at higher resolution. Excessive EKE in stormtrack exit, made worse at higher resolution.

134 views • 5 slides