ROBERT
JAMES GURNEY
Director of NERC Environmental Systems Science Centre University of Reading |
Abundant
water at the Earth's surface in all three phases
(ice, water, water vapour) is one of the key factors that makes the
Earth unique in the Solar System. Water is essential for life,
and is a key component of the Earth's energy and carbon cycles.
Despite this, there are still great uncertainties in our knowledge of
the exchanges of water. The distribution of water vapour in the
atmosphere can largely be determined from the atmospheric dynamics, but
the phase changes via processes of condensation and evaporation,
that result for instance in clouds, are not always so easily
modelled. At the land surface, local heterogeneity means that the
coupling of the terrestrial and atmospheric components of the water
cycle is only known imperfectly, and leads to further uncertainties of
the impacts of changes in land surface characteristics. Remote
sensing has often been suggested to improve our knowledge of the
hydrological cycle, but the benefits promised have only partly been
met, and there are areas where little progress has been made.
Only by using observations with global models will the uncertainty be
reduced. New global models with very high spatial resolution, new
observations and new ways of using the latest computing technology to
bring these together should finally allow progress to be made with
understanding this key component of the Earth system.