Menulis ulang definisi dari suatu konsep

Menghafal nama-nama ibukota negara

Menjelaskan hukum gravitasi

Menjalankan langkah-langkah untuk menyusun laporan keuangan

Decision

New Knowledge

Validated Knowledge

Rules, Lessons, Procedures

Mengurangi biaya operasional perusahaan

Mengurangi jumlah informasi yang diperlukan untuk pengambilan keputusan

Mengandalkan algoritma untuk membuat keputusan secara otomatis

Meningkatkan efektivitas pengambilan keputusan

Easterly

Winds

There

is no wind motion at all at the Equator.

Westerly

Winds

Southerly

winds

Northerly

winds

It

is not important for ocean productivity – in fact upwelling reduces ocean

productivity.

It

brings nutrient-rich water from the deep oceans towards the surface.

It

brings water rich in dissolved gases from the deep oceans towards the surface.

Ekman

transport integrated over the Ekman layer occurs at ~90° to the right in the

Southern Hemisphere.

Moving

water is deflected to the left in the Southern Hemisphere (or right in the Northern Hemisphere) by the coriolis

force.

Net

Ekman transport over the Ekman layer occurs at approximately 90° to the wind direction

The

effects of a wind stress on the ocean surface are transmitted down through the

water column by the action of turbulent eddies that are themselves generated by

the wind.

The

depth to which the effects of wind are felt is inversely proportional to the

Coriolis force magnitude (deeper near the equator and shallower away towards

the poles).