More than one - sixth of the world's population live in glacier - or snowmelt - fed river basins and will be affected by the seasonal shift in streamflow, an increase in the ratio of winter to annual flows, and possibly the reduction in low flows caused by decreased glacier extent or
snow water storage (high confidence)[3.4.1, 3.4.3].
It will monitor runoff, precipitation, evapotranspiration,
snow water storage, soil moisture, groundwater recharge, and sediment yield, thereby reducing our knowledge gaps regarding the effects of forest management on the water cycle.
Not exact matches
That's a problem because
snow is the state's natural
water storage, keeping it locked up until it melts in the warmer months, topping up reservoirs.
Projected changes in temperature will have large effects on how
water enters Montana (e.g., as rain or
snow), how it is distributed among major
storage pools, and how it moves or changes from one component of the
water cycle to another.
«California's dams and
water storage facilities are built to handle the
snow melt as it happened in the past.
Even where increases are projected, there can be short - term shortages due to more variable streamflow (because of greater variability of precipitation), and seasonal reductions of
water supply due to reduced
snow and ice
storage.
Temperature directly influences mountain
snow pack, which provides natural
storage of precipitation during cold winter months until it melts and provides
water in the form of runoff as temperatures warm.