Disagreement among global cloud distributions from CALIOP, passive satellite sensors and general circulation models

TL;DR

This study compares cloud detection from CALIOP lidar, passive satellite sensors, and climate models, revealing discrepancies in cloud detection and vertical distribution, especially over land and tropical regions, highlighting the limitations of passive sensors.

Contribution

It clarifies which cloud subsets are reliably detected by passive sensors versus active sensors and evaluates the realism of climate models against CALIOP observations.

Findings

CALIOP detects more clouds than passive sensors, especially over land.

Passive sensors show large disagreements in tropical subsidence regions.

Climate models do not consistently improve with active sensor data.

Abstract

Cloud detection is the first step of any complex satellite-based cloud retrieval. No instrument detects all clouds, and analyses that use a given satellite climatology can only discuss a specific subset of clouds. We attempt to clarify which subsets of clouds are detected in a robust way by passive sensors, and which require active sensors. To do so, we identify where retrievals of Cloud Amounts (CAs), based on numerous sensors and algorithms, differ the most. We investigate large uncertainties, and confront retrievals from the CALIOP lidar, which detects semitransparent clouds and directly measures their vertical distribution, whatever the surface below. We document the cloud vertical distribution, opacity and seasonal variability where CAs from passive sensors disagree most. CALIOP CAs are larger than the passive average by +0.05 (AM) and +0.07 (PM). Over land, the +0.1 average difference rises to +0.2 over the African desert, Antarctica and Greenland, where large passive disagreements are traced to unfavorable surface conditions. Over oceans, CALIOP retrievals are closer to the average of passive retrievals except over the ITCZ (+0.1). Passive CAs disagree more in tropical areas associated with large-scale subsidence, where CALIOP observes a specific multi-layer cloud population: optically thin, high-level clouds and opaque (z>7km), shallow boundary layer clouds (z<2km). We evaluate the CA and cloud vertical distribution from 8 General Circulation Models where passive retrievals disagree and CALIOP provides new information. We find that modeled clouds are not more realistic where cloud detections from passive observations have long been robust, than where active sensors provide more reliable information.