Laserfiche WebLink
<br />1.16 <br /> <br />Z c.) <br />ZSO <br /> <br /> <br /> <br />ZOI <br /> <br /> \ I I <br /> \ I i ~ ,/' "'" <br /> \ I 'n <br /> I , r'. r' <br /> p , <br /> I \ 1 <br /> ~ <br /> I .; I.~ <br />so 100 II 0.1 n 0.1 0 0.01 '0.2 -0.1 0 <br />be.) II (III ,'1) ip (. ,'1) <1T (10 " (I) <br /> p <br /> <br />ISO <br /> <br />100 <br /> <br />so <br /> <br />o <br />o <br /> <br />Fi~ 1.8. The calculated convective field over snow surface with 250 m convective layer depth, <br />0.7 m s-l wind velocity and 0.1 g m-J liquid water content and -50C temperature at the top boundary. <br />There is no temperature difference between the'air and the snow surface at the lower boundary. <br /> <br />: r., ~T' It! <br />.~ ^ ."'" <br />IIlO I ~ <br /> - - <br /> ! I I <br />l!;ll <br />'M <br /> \.. 0' <br /> . ~ <br />:$0 \ I <br />:Ill <br />'51 \ I \ <br />\II <br />50 I <br />IJ <br />0 . Int ISO ,., II IJ,' IJ, Z IJ n.' IJ n,IlOJ -0.' -IJ,IJS IJ <br /> b (.. .~ (. ."', Ip (. .", &T (lr) ,. (I) <br /> <br /> <br /> <br />Figl4re 1.9. As in Fig. 8, this convective field has no heat flux coming from the snow surface. The <br />depth of this field is 450 m with 0.7 m s-l wind. The liquid water content and temperature at the <br />top boundary are 0.05 9 m-J and _150C, respectively. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br />