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Table of Contents - The Atmospheric Studies Group at TRC

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Section 8: CALMET Model Files<br />

<strong>Table</strong> 8-4 (Continued)<br />

Input <strong>Group</strong> 6 - Mixing Height, Temper<strong>at</strong>ure, and Precipit<strong>at</strong>ion Parameters<br />

Variable Type Description Default Value<br />

ZIMAXW real Maximum overw<strong>at</strong>er mixing height (m) (Not used if<br />

observed overw<strong>at</strong>er mixing heights are used)<br />

ZIMINW real Minimum overw<strong>at</strong>er mixing height (m) (Not used if<br />

observed overw<strong>at</strong>er mixing heights are used)<br />

IAVEZI integer Conduct sp<strong>at</strong>ial averaging <strong>of</strong> mixing heights (0=no,<br />

1=yes)<br />

MNMDAV integer Maximum search distance (in grid cells) in the sp<strong>at</strong>ial<br />

averaging process. <strong>The</strong> square box <strong>of</strong> cells averaged is<br />

2 x MNMDAV in length.<br />

HAFANG real Half-angle <strong>of</strong> upwind-looking cone for sp<strong>at</strong>ial<br />

averaging (deg.)<br />

ILEVZI integer Layer <strong>of</strong> winds used in upwind averaging <strong>of</strong> mixing<br />

heights. (Must be between 1 and NZ.)<br />

IMIXH integer<br />

Method to compute the convective mixing height<br />

1: Maul-Carson for land and w<strong>at</strong>er cells<br />

-1: Maul-Carson for land cells only - OCD mixing<br />

height overw<strong>at</strong>er<br />

2: B<strong>at</strong>chvarova and Gryning for land and w<strong>at</strong>er cells<br />

-2: B<strong>at</strong>chvarova and Gryning for land cells only OCD<br />

mixing height overw<strong>at</strong>er<br />

THRESHL real Threshold buoyancy flux required to sustain<br />

convective mixing height growth overland (expressed<br />

as a he<strong>at</strong> flux per meter <strong>of</strong> boundary layer i.e. W/m3)<br />

THRESHW real Threshold buoyancy flux required to sustain<br />

convective mixing height growth overw<strong>at</strong>er (expressed<br />

as a he<strong>at</strong> flux per meter <strong>of</strong> boundary layer i.e. W/m3)<br />

ITWPROG integer<br />

Option for overw<strong>at</strong>er lapse r<strong>at</strong>es used in convective<br />

mixing height growth<br />

0 : use SEA.DAT (or default constant) lapse r<strong>at</strong>es<br />

1 : use prognostic lapse r<strong>at</strong>es (only if IPROG>2)<br />

3000.<br />

50.<br />

1<br />

1<br />

30.<br />

1<br />

1<br />

0.05<br />

0.05<br />

1<br />

(Input <strong>Group</strong> 6 Continued)<br />

8-49

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