|
Niwot Ridge LTER Snow Report for September 2002 An "end of the official water year" report is not usually done, but
being an unusual year this may be of interest to some.
The following table gives the % of average (1971-2000) snowpack SWE and precipitation
for April 30, 2002, and the % of average
precipitation on September 30, 2002 for all Colorado basins (as listed by the
NRCS SnoTel network).
April 30 values are presented, even though April 1 is the standard date
marking maximum snowpack in the western US, because the Colorado snowpack
usually increases through April, unlike many of the more western states.
September 30th precipitation is given because it is the end of the water year.
Some preliminary comments:
Measures of drought in Colorado would include any combination of many factors (duration
of below average snowpack (which is often more important than rainfall), annual
precipitation, areal extent, soil moisture pre-conditions, seasonality
of precipitation occurrence). Drought indicies, such as the SPI and PDSI,
give a measure of drought severity by incorporating many such fators.
Other considerations of drought assesment include the relative porportion
of precipitation that was sequestered as snowpack. For example when %SWE is less than %PPT, it
indicates factors other than lack of precipitation
are reducing the snowpack (warmer temperatures, lower
reltive humidity, higher ablation rates, etc).
In addition to the meteorological, or hydrological, approach to drought, there is also
the social, or adminstrative aspect. For example, if 100% of the
water rights are used in a year, that defines a drought year to some water managers.
(This suggests that through devlopment and legislation, the state
could - may have already - legislatied itself into drought conditions even during
normal years).
The complex nature of drought, then, may explain the apparent contradictions
or quick "jumps" from normal to drought conditions, particularly as reported
by the media. Thus it may depend upon
who is evaluating the conditions, what their main concerns are, and whether they are
speaking meteorologically, or legislatively.
The past five years data is presented because of media reports of drought durations
this long in SW Colorado, and of up to four years for the rest of Colorado.
Notice that 2002 has many of the drought idicators: wide areal extent (the entire state),
low %SWE to %PPT ratio, and very low total precipitation.
A short summary:
1998: normal to above, especially snowpack, for entire state.
1999: above average annual precipitation statewide, but below average
snowpack except for NE Colorado mountains (S. Platte, Larmie/N Platte).
2000: below average snowpack central and north, and much
below in the south.
2001: above average to average snowpack and precipitation in south, and below in north.
2002: well below averge snowpack and precipitation statewide.
2002 2001 2000 1999 1998
Basin Apr30 9/30 Apr30 9/30 Apr30 9/30 Apr30 9/30 Apr30 9/30
%SWE %PPT %PPT %SWE %PPT %PPT %SWE %PPT %PPT %SWE %PPT %PPT %SWE %PPT %PPT
Gunnison 22 63 64 78 87 87 58 78 85 94 98 111 130 106 94
Upper Colo 30 65 66 80 86 87 80 92 95 92 96 104 104 96 94
S. Platte 34 60 67 87 89 92 94 98 95 120 112 119 109 97 72
Lar/N Platte 48 69 67 74 87 80 92 100 98 100 104 102 92 92 95
Yampa/White 38 68 70 72 87 82 76 95 96 94 103 103 103 100 93
Arkansas 21 55 58 91 93 96 68 92 94 92 107 115 116 106 104
Up Rio Gr. 9 46 48 118 114 98 32 71 64 82 108 119 105 106 96
San M., Dolor. 8 48 52 100 108 96 46 72 71 82 105 124 99 96 95
San Juan, Animas
Return to Snow Report Page |
| This material is based upon work supported by the National Science Foundation under Cooperative Agreement #DEB-9810218. Any opinions, findings, conclusions, or recommendations expressed in the material are those of the author(s) and do not necesarily reflect the views of the National Science Foundation. Please contact lternwt@colorado.edu with questions, comments, or for technical assistance regarding this web site. |