When subjected to a horizontal temperature difference, a fluid layer with a
free surface becomes unstable and hydrothermal waves develop in the bulk.
Such a system is modelled by two coupled amplitude equations of the one-dim
ensional, complex, cubic Ginzburg-Landau type. By transposing the method de
veloped for one CGL3 equation, we obtain several new exact solutions expres
sed by closed-form, single-valued, analytic expressions. Some of them are t
he analogues of the famous amplitude hole solution of Bekki and Nozaki.