Rainfall and Cloud Dynamics in the Andes: A Southern Ecuador Case Study

<table class="table-group" id="tab6"><tr><td><table class="table"><tr><td class="thead-hr" colspan="2"><hr/></td></tr><tr class="thead"><td class="align_left">Approach</td><td class="align_center">Concordance (%)</td></tr><tr><td class="thead-hr" colspan="2"><hr/></td></tr><tr><td class="align_left">CF</td><td class="align_center">17.05</td></tr><tr><td class="align_left">LWP</td><td class="align_center">19.52</td></tr><tr><td class="align_left">ZMIT</td><td class="align_center">16.71</td></tr><tr><td class="align_left">MLRM</td><td class="align_center">46.88</td></tr><tr><td class="align_left">CFM</td><td class="align_center">53.67</td></tr><tr class="table-tr"><td colspan="2"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

Concordance of seasonal regimens of cloud frequency, liquid water path, average cloud top height, multiple linear regression model of rainfall, and PCA cloud frequency model of rainfall against Célleri’s regionalization.

Advances in Meteorology

tab6

Table 6

Table 6: Rainfall and Cloud Dynamics in the Andes: A Southern Ecuador Case Study 