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Table 3 below gives the temperature and dewpoint for a rising air parcel with a surface temperature of $T_{sfc}=13_{?}C$ and a surface dewpoint of $T_{dsfc}=5_{?}C$. (Note that, since $T_{sfc}>T_{d,sfc}$. we know the air parcel is subsaturated at the surface.) Given this information, fill in the missing temperature and dewpoint values for the air parcel at 0.5 $km$ height increments, up to and including a height of $3.0km$ above the surface. Note that, just like you must halve the values of the DALR and MALR to apply them in $0.5km$ increments of height, you must halve the dewpoint lapse rate to apply it in $0.5km$ increments of height. The dewpoint lapse rate becomes $1_{?}C/0.5km$. You should find the air parcel's LCL within the table. Use MALR $=6_{?}C/km$ to calculate temperature and dewpoint values above the air parcel's LCL. The temperature and dewpoint have been given at $2.0km$ and $3.0km$ above the surface for you to check your answers. If your calculations do not lead to these given temperatures and dewpoints. re-do your work, checking the values of your halved lapse rates and making sure you are applying them correctly at and around the LCL. Table 3: Air parcel temperature and dewpoint at $0.5km$ increments of height above the surface, for an air parcel with temperature $13_{?}C$ and dewpoint $5_{?}C$ at the surface
Table 3: Air parcel temperature and dewpoint at $0.5km$ increments of height above the surface, for an air parcel with temperature $13_{?}C$ and dewpoint $5_{?}C$ at the surface

Solution:To determine the temperature and dewpoint of the rising air parcel at different heights, we need to use the following steps:Calculate the lif

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