The continuum exoplanet transit photometry depth is approximately the opaque projected area ratio, assuming a corrected or negligible limb darkening contribution:For a Sun-sized host, . The natural size analogue is Jupiter, not Earth.
The expected bulk constituent is molecular hydrogen, with helium next most abundant for a retained primary planetary atmosphere. The water band detects a strong trace absorber; it does not imply that water is the dominant gas. This interpretation assumes a conventional H/He gas giant; the measured radius by itself is not a measurement of mass or composition.
Interpret the quoted band amplitude as an absolute transit-depth increment , or parts per million. For a thin atmospheric annulus of extra height , the atmospheric spectral-feature amplitude isLet the water band span atmospheric scale heights, so . For a nearly isothermal atmosphere with constant gravity and mean molecular weight , . The temperature from a transmission-band amplitude is thereforeHere refer to the chosen Jupiter reference layer. Assuming , an H/He exoplanet atmosphere with , and a clear strong band with , gives and . Equivalently, a Jovian reference with has , giving .
The assumptions are hydrostatic, approximately isothermal limb gas, constant gravity, negligible cloud truncation, H/He composition, and an effective opacity contrast yielding about five scale heights. In an ideal clear limb, follows from the slant optical depth of an isothermal atmosphere. The data fix , not separately: the temperature is conditional on the band opacity contrast and composition. For – with the same composition and gravity, the estimate is about –.
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