Large-scale models such as GEOS-5 typically calculate grid-scale fractional cloudiness through a PDF parameterization of the sub-gridscale distribution of specific humidity. The GEOS-5 moisture routine uses a simple rectangular PDF varying in height that follows a tanh profile. While below 10 km this profile is informed by moisture information from the AIRS instrument, there is relatively little empirical basis for the profile above that level. ATTREX provides an opportunity to refine the profile using estimates of the horizontal variability of measurements of water vapor, total water and ice particles from the Global Hawk aircraft at or near the tropopause. These measurements will be compared with estimates of large-scale cloud fraction fr...
International audience[1] Using NASA's A-Train satellite measurements, we evaluate the accuracy of c...
A deeper understanding of how clouds will respond to a warming climate is one of the outstanding cha...
On 27 August 2013, during the Studies of Emissions and Atmospheric Composition, Clouds and Climate C...
Water vapor in the lower stratosphere was measured in situ by two aluminum oxide hygrometers mounted...
International audienceWe have developed a Lagrangian air-parcel cirrus model (LACM), to diagnose the...
Publisher's version (útgefin grein)In situ, airborne and satellite measurements are used to characte...
A deeper understanding of how clouds will respond to a warming climate is one of the outstanding ch...
International audienceIn the tropics, deep convection is the major source of uncertainty in water va...
Temperature and water vapor variations due to clouds in the tropical tropopause layer (TTL) are inve...
Changes in the amount of stratospheric water vapor can affect both the chemistry and climate in the ...
Evaluating the representation of processes controlling tropical and subtropical tropospheric relativ...
The detection, distribution, and dynamics of atmospheric water on Earth was examined. How the high l...
International audienceSimulations of overshooting, tropical deep convection using a Cloud Resolving ...
International audience[1] Using NASA's A-Train satellite measurements, we evaluate the accuracy of c...
A deeper understanding of how clouds will respond to a warming climate is one of the outstanding cha...
On 27 August 2013, during the Studies of Emissions and Atmospheric Composition, Clouds and Climate C...
Water vapor in the lower stratosphere was measured in situ by two aluminum oxide hygrometers mounted...
International audienceWe have developed a Lagrangian air-parcel cirrus model (LACM), to diagnose the...
Publisher's version (útgefin grein)In situ, airborne and satellite measurements are used to characte...
A deeper understanding of how clouds will respond to a warming climate is one of the outstanding ch...
International audienceIn the tropics, deep convection is the major source of uncertainty in water va...
Temperature and water vapor variations due to clouds in the tropical tropopause layer (TTL) are inve...
Changes in the amount of stratospheric water vapor can affect both the chemistry and climate in the ...
Evaluating the representation of processes controlling tropical and subtropical tropospheric relativ...
The detection, distribution, and dynamics of atmospheric water on Earth was examined. How the high l...
International audienceSimulations of overshooting, tropical deep convection using a Cloud Resolving ...
International audience[1] Using NASA's A-Train satellite measurements, we evaluate the accuracy of c...
A deeper understanding of how clouds will respond to a warming climate is one of the outstanding cha...
On 27 August 2013, during the Studies of Emissions and Atmospheric Composition, Clouds and Climate C...