Furthermore, the Indian monsoon is clearly demonstrated in the water vapor map. It should be noted that the water vapor content retrieved from the POLDER data has been validated with AERONET measurements.S. MukaiI. SanoT. HirataB. N. Holben...
Russian scientists from the Space Research Institute of the Russian Academy of Sciences and the Moscow Institute of Physics and Technology (MIPT), together with their French and American colleagues, have created a 'map' of the distribution of water vapour in Mars' atmosphere. Their research include...
, and R. Joyce (2008), Water vapor, cloud liquid water paths, and rain rates over northern high latitude open seas, J. Geophys. Res., 113, D05205, doi:10.1029/2007JD009040. Author Information 1 Rosenstiel School of Marine and Atmospheric Sciences, Univ. of Miami, Miami, Florida, USA ...
(22 ka to 10 ka) monsoons were predominantly influenced by rising water vapor due to increasing sea surface temperature, whereas in the Holocene (10 ka to 0 ka) cloud feedback was more important. These results are consistent with another transient simulation, thus increasing confidence ...
在这些数据中，空间的3个纬度通常是经度、纬度和气压层，即高空等压面数据。例如，高度索引从低到高可以...
Data Records The isotopic and meteorological data are archived at Data Citation 1 and an interactive map of these data are available at http://vapor-isotope.yale.edu/. Variable Table The isotopic and meteorological data are recorded in comma separated ascii- format in csv files, and the meta ...
The Los Alamos National laboratory (LANL) scanning Raman lidar has been used to measure multi-dimensional water vapor fields and now is being used to map l... DI Cooper,WE Eichinger,J Archuleta,... - Conference on Biometeorology & Aerobiology 被引量: 0发表: 2000年 Length–mass relationships...
Within the exchanger, the vapor is condensed into liquid of the same temperature, transferring heat to the water flowing across the channels adjacent to the vapor channels. The liquid then enters the liquid header located right below the vapor header, due to the gravity caused by the height ...
whereElakeis the lake evaporation rate (mm d−1); ∆ is the slope of the saturation vapor pressure curve (kPa °C−1);Rnis the net radiation (MJ m−2d−1);δUis the heat storage change of the water body (MJ m−2d−1);aandbare the wind function coefficients (and are ...
Therefore, an under- standing of processes controlling isotope ratios in water vapor during a recent increase in open water and atmospheric humidity, as may be found in an unusually intense, warm-season Arctic cyclone, provides context to help explain the water isotope ratios during past periods ...