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Yampa: <br />Most HCI variable are weak and non-usable with only (at best) some minor <br />correlation to the PDO however, this relationship may not be of use for multi-year <br />analysis. <br />Table 10. Summary of Dec.-Mar. Multi (2-year) Precipitation/HCI Relationships for the <br />Colorado/Gunnison/Yampa-White basins (‘X’ indicates a relatively strong relationship and ’O’ <br />indicates a relatively weak relationship). <br />PDOMEISOINino 3.4 NAOAMO <br />Upper Colo. <br />X <br />Middle Colo. X <br />Eagle <br />X <br />Roaring Fork XXX <br />Gunnison <br />XX <br />Uncompaghre <br />WhiteX <br />Yampa <br />X <br />April to June Precipitation: <br />Upper Colorado (River above Kremmling): <br />The leading modes of the NAO have minor connections but, are unfortunately the <br />best precipitation depiction possible. Minor connection with ENSO exists however, a <br />look at the actual connection do not appears to be useful unless the ENSO value <br />(preferably the SOI) is strongly shifted one way or the other. <br />Middle Colorado (River from Kremmling to Glenwood Springs): <br />The leading modes of the NAO have minor connections but, are unfortunately the <br />best precipitation depiction possible. Minor connection with ENSO exists however, a <br />look at the actual connection do not appears to be useful unless the ENSO value <br />(preferably the SOI) is strongly shifted one way or the other. <br />Eagle: <br />There is some non-random connection with ENSO (preferably the SOI) with El <br />Nino years leaning towards more precipitation and vice-versa for the 2-year spring <br />average. <br />37 <br />