Tropical Warm Pool - International Cloud Experiment (TWP-ICE)
21 January 2006 - 13 February 2006
Lead Scientist: Peter May
This experiment was undertaken over a four week period in early 2006. January/February corresponding to the wet phase of the Australia monsoon. This season was selected because, despite Darwin’s coastal location, the convection that occurs over and near Darwin at this time is largely of maritime origin with a large fetch over water. Based on previous experiments, the convection appears typical of maritime convection with widespread convection that has complex organization, but is not as deep or as intense as continental or coastal convection. Therefore, it was expected that the convection and cloud characteristics would be representative of conditions typical for wide areas of the tropics.
Observations of cloud properties were provided by an extensive set of in situ and remote sensing instruments. The Darwin ARM site provided continuous measurements of cloud properties through remote sensing retrievals. A second set of instruments was deployed on a ship in the Timor Sea, approximately 100 km northwest of Darwin. Added to these surface-based observations were several research aircraft including the NASA WB-57, the DOE Proteus, the DLR Falcon and the Geophysica, as well as three aircraft provided by Airborne Research Australia (ARA): the Egrett, King Air and Dimona. These aircraft fulfilled a variety of observational requirements to address the science goals. The strategy for utilizing these aircraft included obtaining in situ observations of cirrus properties combined with remote sensing observations obtained from above and below the clouds. In addition, a boundary layer aircraft was used to characterize radiative and turbulent fluxes in the boundary layer.
The boundary layer observations were part of the effort to characterize the convective environment in which the cirrus are formed. Other observational components geared toward describing the environment included a network of radiosonde stations encircling Darwin, a pair of precipitation radars, wind profilers, and surface flux stations. Darwin is a coastal site and it was important to characterize the oceanic region off the Australia coast. For this purpose, the CSIRO research vessel Southern Surveyor was stationed in the Timor Sea to the northwest of Darwin. This ship served as a launch site for sondes, to complete the ring around Darwin and also carried surface flux instruments. In addition to flux observations, remote sensing instruments were also planned for the ship. The addition of these instruments provided a complete second surface site. This capability increased the likelihood of obtaining good coordinated surface/aircraft observations.
The occurrence of tropical clouds in the form of shallow non-precipitating cumulus to deep precipitating cumulonimbus with extensive anvils have a significant and fundamental impact on the atmospheric energy balance. Understanding the properties of these clouds and parameterizing their impact within climate prediction models is one of the major challenges facing the international community. It is well recognized that the representation of these process is a major uncertainty in our ability to represent and predict climate. In that context modeling activities, including the application of Cloud Resolving and Single Column Models as well as a suite of Numerical Weather Prediction models, formed a major component of the experiment activities. Those activities included pre-experiment model evaluation, NWP support during experiment and a large post-experiment program that made use of the collected data in evaluating and improving the representation of cloud, convective and radiative processes in the models.
The ARM project takes long term observations to provide data to address the cloud characteristics and their radiative effects. TWP-ICE provided important in situ data to both verify the remote retrievals and provide high resolution in situ data that cannot be remotely sensed. The experiment also provided an invaluable description of the convective environment. Together, the observations of cloud properties and the atmospheric state make this a data set unique for improving cloud parameterizations in the tropics.
Ovchinnikov M, K Lim, V Larson, M Wong, K Thayer-Calder, and S Ghan. 2016. "Vertical overlap of probability density functions of cloud and precipitation hydrometeors." Journal of Geophysical Research: Atmospheres, 121(21), 10.1002/2016JD025158.
Kumar VV, A Protat, C Jakob, CR Williams, S Rauniyar, GL Stephens, and PT May. 2016. "The Estimation of Convective Mass Flux from Radar Reflectivities." Journal of Applied Meteorology and Climatology, 55(5), 10.1175/JAMC-D-15-0193.1.
Liu Z, A Muhlbauer, and T Ackerman. 2015. "Evaluation of high-level clouds in cloud resolving model simulations with ARM and KWAJEX observations." Journal of Advances in Modeling Earth Systems, 7(4), 10.1002/2015MS000478.
Zhang GJ, X Wu, X Zeng, and T Mitovski. 2015. "Estimation of convective entrainment properties from a cloud-resolving model simulation during TWP-ICE." Climate Dynamics, , doi:10.1007/s00382-015-2957-7.
Lebo ZJ, CR Williams, G Feingold, and VE Larson. 2015. "Parameterization of the Spatial Variability of Rain for Large-Scale Models and Remote Sensing." Journal of Applied Meteorology and Climatology, 54(10), 10.1175/JAMC-D-15-0066.1.
Mrowiec AA, OM Pauluis, AM Fridlind, and AS Ackerman. 2015. "Properties of a Mesoscale Convective System in the Context of an Isentropic Analysis." Journal of the Atmospheric Sciences, 72(5), 10.1175/JAS-D-14-0139.1. ONLINE.
Kumar VV, C Jakob, A Protat, CR Williams, and PT May. 2015. "Mass-Flux Characteristics of Tropical Cumulus Clouds from Wind Profiler Observations at Darwin, Australia." Journal of the Atmospheric Sciences, 72(5), 10.1175/JAS-D-14-0259.1.
Um J, GM McFarquhar, Y Hong, S Lee, C Jung, R Lawson, and Q Mo. 2015. "Dimensions and aspect ratios of natural ice crystals." Atmospheric Chemistry and Physics, 15(7), 10.5194/acp-15-3933-2015.
Edman JP and DM Romps. 2015. "Self-consistency tests of large-scale dynamics parameterizations for single-column modeling." Journal of Advances in Modeling Earth Systems, 7(1), 10.1002/2014MS000378. ONLINE.
Suhas E and G Zhang. 2015. "Evaluating convective parameterization closures using cloud-resolving model simulation of tropical deep convection." Journal of Geophysical Research: Atmospheres, 120(4), 10.1002/2014JD022246.
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Campaign Data Sets
|IOP Participant||Data Source Name||Final Data|
|Richard Austin||Twin Otter Radar||Order Data|
|Jason Beringer||Surface Flux Analysis||Order Data|
|Ann Fridlind||CRM Intercomparison||Order Data|
|Jorg Hacker||Airborne Surface Fluxes||Order Data|
|Hartmut Hoeller||Lightning Detection Network||Order Data|
|Christian Jakob||Radiosondes||Order Data|
|Yanluan Lin||AGCM Intercomparison||Order Data|
|Guosheng Liu||Liu cloud ice water||Order Data|
|Chuck Long||Surface Flux Analysis||Order Data|
|James Mather||PARSL||Order Data|
|Greg McFarquhar||Proteus Microphysics||Order Data|
|Mario Mech||Microwave Radiometer Profiler||Order Data|
|Peter Minnett||Maeri||Order Data|
|Patrick Minnis||visst||Order Data|
|R. Reynolds||Surface Flux - Ship||Order Data|
|Tim Tooman||Proteus||Order Data|
|David Turner||MWR Retrievals||Order Data|
|Jim Whiteway||Twin Otter Lidar||Order Data|
|Christopher Williams||S-band Radar||Order Data|
|Steven Wofsy||Proteus CO2 Mixing Ratios||Order Data|
|Shaocheng Xie||Constrained Variational Objective Analysis Data||Order Data|