What determines the number of possible suborbitals?

the principal energy level

the shape of the orbital

the energy of the orbital

the ground state

The principle energy level hope it helps.

Answerthe global climate during the paleogene departed from the hot and humid conditions of the late mesozoic era and began a cooling and drying trend which dispite having been periodically disrupted by warm periods such as the paleocene-eocene thermal maximum, persists today;

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