The Subantarctic and the Southern Ocean are regions where there are sparse ground-based and in-situ cloud measurements. While satellite measurements provide continuous spatial and temporal coverage, they are generally not capable of observing low-level clouds and the cloud base, which are critical for understanding the radiative energy budget. Results from general circulation models show bias in the shortwave radiation in this region, related to representation of clouds. As part of the Cloud and Aerosol project of the New Zealand Deep South National Science Challenge (DSC) we aim to collect and analyse cloud measurements from shipborne and ground-based deployments of several meteorological instruments: a near-infrared ceilometer, a micro ra...
Southern Ocean (SO) shortwave (SW) radiation biases are a common problem in contemporary general cir...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Current general circulation models are affected by biases in simulated clouds in the Southern Ocean ...
The Southern Ocean is characterised by sparse ground-based and in-situ atmospheric measurements. Whi...
One of the primary objectives of the New Zealand Earth System Model (NZESM) is to reduce shortwave r...
One of the primary objectives of the New Zealand Earth System Model (NZESM) is to reduce shortwave r...
International audienceDue to its remote location and extreme weather conditions, atmospheric in situ...
International audienceDue to its remote location and extreme weather conditions, atmospheric in situ...
Due to its remote location and extreme weather conditions, atmospheric in situ measurements are rare...
Due to its remote location and extreme weather conditions, atmospheric in situ measurements are rare...
Due to its remote location and extreme weather conditions, atmospheric in situ measurements are rare...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Southern Ocean (SO) shortwave (SW) radiation biases are a common problem in contemporary general cir...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Current general circulation models are affected by biases in simulated clouds in the Southern Ocean ...
The Southern Ocean is characterised by sparse ground-based and in-situ atmospheric measurements. Whi...
One of the primary objectives of the New Zealand Earth System Model (NZESM) is to reduce shortwave r...
One of the primary objectives of the New Zealand Earth System Model (NZESM) is to reduce shortwave r...
International audienceDue to its remote location and extreme weather conditions, atmospheric in situ...
International audienceDue to its remote location and extreme weather conditions, atmospheric in situ...
Due to its remote location and extreme weather conditions, atmospheric in situ measurements are rare...
Due to its remote location and extreme weather conditions, atmospheric in situ measurements are rare...
Due to its remote location and extreme weather conditions, atmospheric in situ measurements are rare...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Southern Ocean (SO) shortwave (SW) radiation biases are a common problem in contemporary general cir...
Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (...
Current general circulation models are affected by biases in simulated clouds in the Southern Ocean ...