We discuss spatio-temporal pattern formation in two separate thermal
convective systems. In the first system, hydrothermal waves (HTW) are modeled
numerically in an annular channel. A temperature difference is imposed across
the channel, which induces a surface tension gradient on the free surface of
the fluid, leading to a surface flow towards the cold side. The flow pattern is
axially symmetric along the temperature gradient with an internal circulation
for a small temperature difference. This axially symmetric flow (ASF) becomes
unstable beyond a given temperature difference threshold, and subsequently,
symmetry-breaking flow, i.e., rotational oscillating waves or HTW, appears. For
the second system, Rayleigh-B'enard convection (RBC) is experimentally studied
in the non-turbulent regime. When a thin film of liquid is heated, the
competing forces of viscosity and buoyancy give rise to convective
instabilities. This convective instability creates a spatio-temporal
non-uniform temperature distribution on the surface of the fluid film. The
surface temperature statistics are studied in both these systems as order' and disorder’ phase separates. Although the mechanisms that give rise to
convective instabilities are different in both cases, we find an agreement on
the macroscopic nature of the thermal distributions in these emergent
structures.

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