Of the so-called atmospheric greenhouse gases, water vapor is the most effective in producing
surface-atmospheric warming. Water-vapor concentrations increase rapidly over the tropical
oceans when sea surface temperatures (SSTs) begin to rise (as in global warming scenarios, for
example). This effect is greatest over the huge "warm pools" of the Pacific Ocean. The water-
vapor content of the atmosphere above the ocean increases by about 1520% for each 1% of
increase in SST. These increasing concentrations of water vapor trap more and more heat, which
causes the ocean's surface temperature to rise even further, thus creating a "super-greenhouse
effect." Unchecked, this feedback mechanism would result in runaway warming. This is not what
is observed, however; even in the "warm pool," SSTs never exceed 304 K (31ºC). This suggests
that some kind of "thermostat" might exist. Furthermore, deep intensive convection over the
tropical oceanwith cloud tops reaching altitudes of 18 to 20 kmonly when SSTs
exceed about 300 K. These observations raise two central questions:
It has been argued that cooling by evaporation from the ocean surface provides such a mechanism.
- Why do maximum SSTs in the tropical oceans remain within a few degrees of the 300 K threshold SST for deep convection?
- What are the restoring forces that limit SST and deep convection to observed tropical Pacific values?
However, observations from space and from the atmospheric boundary layer indicate that this
process is not sufficient. Rather, it may be the very high and cold cirrus clouds, streaming from
tropical thunderstorms, stretching over large areas of the Pacific, and reflecting the incoming solar radiation that, in fact, act as a thermostat (see Figure 1).
The purpose of the Central Equatorial Pacific Experiment (CEPEX) is to investigate this
mechanism. The overall scientific goal of CEPEX is to establish the respective roles of cirrus
radiative effects and surface evaporation in limiting maximum surface temperature in the equatorial Pacific.
Direct in-situ measurement of radiation fluxes, cirrus microphysics, evaporation rates, and water-
vapor distributions must be obtained over a range of SSTs, from regions where SST is just below
the convection threshold temperature to regions where SST exceeds it. Accordingly, the CEPEX
experiment domain will encompass the transition (with respect to SST) region from the central
equatorial Pacific to the tropical south Pacific or the tropical western Pacific "warm pool."
The primary experimental objectives of CEPEX are to:
Multiple platforms (surface, airborne, and space-borne) will be employed to achieve these
objectives (see Figure 2). Observations from high-altitude aircraft above and below the cirrus will
be used to estimate the albedo of cirrus and the radiation energy converging into the cirrus, as well
as the water-vapor distribution above and below the cirrus, the horizontal gradient of cirrus
radiative heating, and the microphysical causes for the brightness of the cirrus. Observations from
a low-level aircraft and a ship will be used to estimate evaporation from the sea surface and its
relationship to SST gradients and how the cirrus regulates solar energy flux to the sea surface. In
addition, upsondes launched from the ship and islands, dropsondes launched from aircraft, surface
buoys, satellite cloud data, and island surface meteorological and radiation sensors will complete
the CEPEX composite observing system (see Figure 3).
- measure, by direct atmospheric observations, the vertical structure of the water-vapor
- measure the effect of cirrus on radiation fluxes over the equatorial Pacific
- measure the east-west gradients of SST and the evaporative and sensible heat-flux from the sea surface along the equatorial Pacific
- measure the east-west gradients of vertical distribution of water-vapor along the equatorial Pacific
- explore the microphysical factors contributing to the high albedo of widespread tropical cirrus layers
CEPEX will be conducted in March 1993 with an operations base in Fiji, immediately following the TOGA-COARE study of the western tropical Pacific Ocean, and will take advantage of many of COARE's observing systems, including several critical ones that will remain in place during the CEPEX field phase. Data from the TOGA (Tropical Ocean Global Atmosphere)- COARE field phase will provide information essential to CEPEX (i.e., understanding the most important forcing mechanisms for maintenance of the warm pool). CEPEX will contribute to the interpretation of TOGA-COARE results by providing coverage for an extended period and over a larger area and by focusing on the thermodynamic cloud forcing mechanism for the regulation of the ocean warm pool.
Back to the Table of Contents