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Terrain slope (degrees)<br />

Terrain slope (degrees)<br />

a.<br />

14-cm SWE<br />

at 0<br />

b.<br />

o a.<br />

14-cm SWE<br />

at 0 slope<br />

b.<br />

o slope<br />

-10<br />

-5<br />

25<br />

20<br />

15<br />

10<br />

5.5<br />

5<br />

0<br />

S<br />

ΔΔ SWE SWE (x) (x)<br />

1.4<br />

0<br />

5<br />

10<br />

162<br />

18 342<br />

198<br />

N<br />

5<br />

0<br />

5<br />

10<br />

ΔΔ SWE SWE (y) (y)<br />

54 306 126<br />

241<br />

90<br />

Terrain Terrain slope (degrees)<br />

100<br />

270<br />

40<br />

450-kg m-3 density<br />

at 0o 450-kg m<br />

slope<br />

-3 density<br />

at 0o slope<br />

S<br />

10<br />

0<br />

ΔΔ Density Density (x) (x)<br />

234<br />

0.08 0.1 0.12 0.14 0.16 0.18 0.2<br />

<strong>Snow</strong> water equivalent (m)<br />

Figure 9. Modeled snow water equivalent (x-axis) for day 110 plotted against terrain slope.<br />

The circles indicate <strong>the</strong> SLTHERM solution points.<br />

-100<br />

N<br />

0<br />

ΔΔ Density Density (y) (y)<br />

Figure 10. (Left) Shaped solution for snow water equivalent for day 110 in <strong>the</strong> sparse forest at 900-m<br />

elevation. (Right) Shaped solution for snow density derived from <strong>the</strong> depth <strong>an</strong>d water equivalent cones.<br />

The arrows at <strong>the</strong> vertices represent <strong>the</strong> maximum (north-south) <strong>an</strong>d minimum (e<strong>as</strong>t-west) Δ SWE (cm)<br />

<strong>an</strong>d Δ density (kg m –3 ), respectively, relative to <strong>the</strong> 0° slope c<strong>as</strong>e. The arrows are not to scale. Corrections to<br />

r=0 on minimum axes are not shown.

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