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Fig. 6 a Daily mean difference of the LRT temperature (∆T LRT) and b the difference of the CPT altitude (∆H LRT) among the three COSMIC GPS-RO datasets.
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The example in Fig. 11 indicates that the two versions of the CDAAC products have some discrepancies when determining the altitudes of CPT and LRT, resulting in inconsistencies of the corresponding CPT and LRT temperatures.
Following the WMO definition, we defined the LRT at the lowest level where the temperature lapse rate (−dT/dz) decreases to 2 K/km and the average of the lapse rate between this and higher levels within 2 km does not exceed 2 K/km.
Beyer et al. [5] could demonstrate that the LRT potential can monotonically increase or decrease with increasing temperature, or it can have a maximum in the temperature range between 5 and 30 °C.
The RISH and CDAAC data produce different behaviors between the temperature and the altitude of CPT and LRT.
These fluctuations affect the determination of a reliable LRT; LRT is detected at a lower altitude and a warmer temperature.
The random regression analysis first showed evidence for individual slopes variability in the relationship between laying date and breeder density in the random part of the model (i.e. IxE for breeder density; model 5: LRT = 10.81, P = 0.004; Table 3; Fig. 4A), but not for individual-by-temperature variability (i.e. no IxE for spring temperature; model 4: LRT = 0.50, P = 0.78; Table 3; Fig. 4B).
'02 - Last call for printed copies of the lrt book.
24 May '02 - Somewhat revised lrt book available.
Man at 66th St. Station of LRT has record of fifty-nine.
We also modified lrt to run on multiple machines simultaneously through the standard MPI interface.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com