OD1_USTH

"Large scale" in GFD is when you can ignore the rotation

• TRUE

• FALSE

• no Coriolis effect

• The Coriolis effect does not vary with latitude

• The Coriolis effect does vary with latitude

• is suitable for global scale

• is suitable for basin scale

• is suitable for small scale

• is suitable for global scale

• is not suitable for basin scale

In equation of motion, w is velocity component in

• x- direction

• y - direction

• z-direction

• weight

horizontal pressure gradients are caused by

• the varying chemical components of water in different regions of the ocean

• the varying temperature of water in different regions of the ocean

• the varying weight of water in different regions of the atmosphere

• the varying weight of water in different regions of the ocean