Forecasts for Hams Fork, Blacks Fork, and Flaming Gorge inflow are in the top five historical observed volumes.
The following conditions influenced this month's forecasts:

Precipitation:
Seasonal October through April precipitation was 130 percent of average in the Upper Green basin. April precipitation was 150 percent of average in the basin as a whole.

Snow:
May 1st snow water equivalent was 160 percent of average in the basin.
--- Upper Green basin snow water equivalent plot.

Streamflow:
April streamflow was near 100 percent of average.

Soil Moisture:
Modeled soil moisture states were below average heading into the winter.

Climate Forecasts:
Climate forecasts were not a factor because there is not a strong correlation between La Nina conditions and winter precipitation in the Upper Green basin.

Forecast Summary:
With the addition of much above average precipitation in April, the seasonal precipitation and snow water equivalent have increased since April 1 and are now much above average for the Upper Green. As a result of the current conditions, the April through July streamflow volume forecasts increased by approximately 10 to 20 percent from the April 1 forecasts. Current forecasts range between 108 and 179 percent of average with a median value of 139 percent. Forecasts for Hams Fork, Blacks Fork, and Flaming Gorge inflow are in the top five historical observed volumes.

The majority of these forecast volumes are in the top three or record of historical observed volumes.
The following conditions influenced this month's forecasts:
Precipitation:
Seasonal October through April precipitation was 135 percent of average in the Yampa/White basin. April precipitation was 160 percent of average in the basin as a whole.

Snow:
May 1st snow water equivalent was 165 percent of average in the basin.
--- Yampa basin snow water equivalent plot.

Streamflow:
April streamflow was near 120 percent of average.

Soil Moisture:
Modeled soil moisture states were near average heading into the winter for the Yampa, Little Snake,and White River basins.

Climate Forecasts:
Climate forecasts were not a factor in the forecasts because there is not a strong correlation between La Nina conditions and winter precipitation in the Yampa/White basin.

Forecast Summary:
With the addition of much above average precipitation in April, the seasonal precipitation and current snow water equivalent have increased since April 1 and are now much above average for the Yampa basin. It is also important to note that the majority of the snotel locations have record snow water equivlent for May 1. As a result of the current conditions, the April through July streamflow volume forecasts have increased by approximately 15 to 25 percent. Current forecasts range between 148 and 216 percent of average with a median value of 193 percent. The majority of these forecast volumes are in the top three or record of historical observed volumes.

Many of these forecast volumes are in the top five historical observed volumes.
The following conditions influenced this month's forecasts:
Precipitation:
Seasonal October through April precipitation was 160 percent of average in the Duchesne basin. April precipitation was 180 percent of average the basin as a whole; however, portions of the basin only received near average precipitation such as the headwaters of Ashley Creek, Big Brush Creek, and Whiterocks.

Snow:
May 1st snow water equivalent was 190 percent of average in the basin.
--- Duchesne basin snow water equivalent plot.

Streamflow:
April streamflow was 120 percent of average.

Soil Moisture:
Modeled soil moisture states were much below average to below average heading into the winter.

Climate Forecasts:
Climate forecasts were not a factor in the forecasts because there is not a strong correlation between La Nina conditions and winter precipitation in the Duchesne basin.

Forecast Summary:
Seasonal precipitation and current snow water equivalent have increased as a result of much above average April precipitation and still remain much above average. As a result of the current conditions, the majority of the April through July streamflow volume forecasts increased by approximately 15 to 20 percent. However, forecasts for Ashley Creek, Big Brush, and Whiterocks remained similiar to the April 1 forecasts due to near average precipitation. Current forecasts range between 108 and 227 percent of average with a median value of 181 percent. Many of these forecast volumes are in the top five historical observed volumes.

Many of these forecast volumes are in the top five historical observed volumes.
The following conditions influenced this month's forecasts:

Precipitation:
Seasonal October through April precipitation was 160 percent of average in the Lower Green basin. April precipitation was 180 percent of average.

Snow:
May 1st snow water equivalent was 160 percent of average in the basin as a whole.
--- Lower Green basin snow water equivalent plot.

Streamflow:
April streamflow was near 100 percent of average.

Soil Moisture:
Modeled soil moisture states were much below to near average heading into the winter.

Climate Forecasts:
Climate forecasts were not a factor in the forecasts because there is not a strong correlation between La Nina conditions and winter precipitation in the Lower Green basin.

Forecast Summary:
Seasonal precipitation and current snow water equivalent have increased as a result of much above average April precipitation and still remain much above average. As a result of the current conditions, the April through July streamflow volume forecasts have increased by approximately 15 to 20 percent from the April 1 forecasts. Current forecasts range between 151 and 190 percent of average with a median value of 167 percent.

Many of these forecast volumes are in the top three of historical volumes, with the forecasts for Lake Granby, Willow Creek Reservoir and Wolford Reservoir at or above the record volumes.

The following conditions influenced this month's forecasts:

Precipitation:
April precipitation was near 175 percent of average overall in the Upper Colorado mainstem basin. However, the uppermost headwaters of the basin received near 190% of average precipitation for the month, while the Eagle River basin had close to 230% of average. Seasonal precipitation (the total since October) increased since last month and now stands at 140 percent of average.

Snow:
May 1st snow water equivalent was near 155 percent of average in the basin as a whole. This is especially significant for this time of year as the snow melt has been delayed and so it is also near 150% of the average seasonal peak. Conditions are even more extreme in the headwaters of the basin where the May 1st snow water equivalent was near 175 percent of average. Many snotel sites throughout the basin have snow water equivalent values that are at record levels when compared to their historical period (20-30 years).
--- Upper Colorado basin snow water equivalent plot

Streamflow:
April streamflow was above average at 125 percent.

Soil Moisture:
Modeled soil moisture states were near to above average heading into the winter.

Climate Forecasts:
Climate forecasts were not a factor because there is not a strong correlation between La Nina conditions and winter precipitation in the Upper Colorado mainstem basin.

Forecast Summary:
All forecast volumes were raised significantly from last month due to the much above average precipitation during April as well as cool temperatures which have delayed the start of the snow melt. This has resulted in near to above record snow pack conditions throughout much of the basin. Current April through July streamflow volume forecasts range between 140 and 190 percent of average with a median value of 155 percent. Current May through July streamflow volume forecasts range between 145 and 200 percent of average with a median value of 165 percent. Many of these forecast volumes are in the top three of historical volumes, with the forecasts for Lake Granby, Willow Creek Reservoir and Wolford Reservoir at or above the record volumes.

The following conditions influenced this month's forecasts:

Precipitation:
Seasonal October through April precipitation was 120 percent of average in the Gunnison basin. April precipitation was 150 percent of average.

Snow:
May 1st snow water equivalent was near 140 percent of average in the Gunnison basin; this is around 120% of the seasonal peak.
--- Gunnison basin snow water equivalent plot

Streamflow:
April streamflow was 100 percent of average.

Soil Moisture:
Modeled soil moisture states were below to near average heading into the winter.

Climate Forecasts:
Climate forecasts were not a factor because there is not a strong correlation between La Nina conditions and winter precipitation in the Gunnison basin.

Forecast Summary:
April precipitation throughout the Gunnison basin was much above average at 150%. Seasonal precipitation for the Gunnison basin rose from last month to 120% of average. May 1st snow water equivalent for the Gunnison was much above average with 140%; whereas the snow water equivalent is 120% of the average seasonal peak. Since there was an increase in the snow water equivalent in the Gunnison basin, the current April through July streamflow volume forecasts rose from last month's forecast. Current April through July streamflow volume forecasts range between 98 and 146 percent of average with a median value of 130 percent.

The following conditions influenced this month's forecasts:

Precipitation:
Seasonal October through April precipitation was 105 percent of average in the entire Dolores basin. April precipitation was 150 percent of average.

Snow:
May 1st snow water equivalent was 95 percent of average in the Dolores basin as a whole; this is about 45% of the seasonal peak.
--- Dolores basin snow water equivalent plot

Streamflow:
April streamflow was 65 percent of average.

Soil Moisture:
Modeled soil moisture states were average to slightly below average heading into the winter.

Climate Forecasts:
The correlation of La Nina and April through July water volumes in the Dolores basin is small that it did not influence the forecast process.

Forecast Summary:
April precipitation throughout the Dolores basin was much above average at 150%. Seasonal precipitation for the Dolores basin rose from last month to 105% of average. May 1st snow water equivalent for the Dolores was average with 95%; whereas the snow water equivalent is 45% of the average seasonal peak. Since the percent of average for both snow water equivalent and seasonal precipitation increased from last month, the current April through July streamflow volume forecasts rose in the Dolores Basin from last month's forecast. Current April through July streamflow volume forecasts range between 72 and 92 percent of average, with a median value of 75 percent.

The following conditions influenced this month's forecasts:

Precipitation:
Seasonal October through April precipitation was 95 percent of average, up 5 percent from last month. April precipitation was 140 percent of average, which was much above average.

Snow:
Current snow water equivalent for the entire basin is 95 percent, which is average. The Animas basin is 100 percent and above Navajo is 90 percent. All three are up from the April 1st percentages.
--- Animas River Basin Snow Plot.
--- Above Navajo Basin Snow Plot.

Streamflow:
Streamflow for the entire San Juan Basin was much below average for April at 60%. Seasonal streamflow since October continued to be much below average at 60%, due to the much below average fall precipitation.

Soil Moisture:
Modeled soil moisture as of November 1st, 2010 was average to below average across the entire San Juan Basin.

Climate Forecasts:
The correlation of La Nina and April through July water volumes in the San Juan basin does suggest slightly drier than average December through May precipitation, but it did not influence the April forecast process.

Forecast Summary:
The April-July forecast volumes changed little from last month and currently range between 60 and 90 percent of average with a median value of 75%.

Differences between the full period forecasts and the residual forecasts may not exactly equal the actual observed volumes due to rounding conventions (see Definitions section).