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Hydrologic sensitivity of watersheds to MPB infestation in the B.C.
Interior
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Hydrology, Maps, and Geographic Data for Watersheds Affected By Mountain Pine Beetle in the Interior of British Columbia
As the mountain pine beetle (MPB) spreads through
the interior of British Columbia, the extent of lodgepole pine mortality
and salvage logging will be significant in many watersheds. Stand
mortality, salvage logging, and road construction each have the
potential to affect hydrologic processes. The following text provides
an introduction to the hydrologic consequences of both the MPB
infestation and salvage operations, sources of information, and links to
a series of maps and tables indicating the extent of lodgepole pine
dominated forest cover types in medium to large watersheds throughout
the interior of British Columbia.
A reduction in forest canopy can result in:
- increased water reaching, stored in, and flowing from hillslopes,
- earlier onset of spring snowmelt,
- increased spring and total annual streamflow volumes,
- changes in summer and fall flows, and
- more rapid streamflow response to storms.
The magnitude of hydrologic change will depend on:
- the severity and time since attack,
- presence, density and extent of understory vegetation,
- the extent of salvage logging within stands and across a watershed,
- the occurrence of fire,
- the physical characteristics of the watershed, and
- the weather.
If attacked stands are left to deteriorate
naturally, hydrologic change will be gradual as trees turn from green to
red, drop their needles, lose fine branches, and eventually fall to the
ground. At the same time, understory vegetation will be releasing due
to increased light levels and reduced competition for nutrients. In
contrast, salvage logging can result in an immediate change to a
hydrologic system. For example, logging will physically remove the dead
standing pine, and therefore eliminate any role they might provide
through shade or canopy interception of precipitation. In addition,
logging can affect the hydrologic system through:
- removal of non-pine species and understory vegetation including coniferous regeneration, shrubs, and herbs,
- changing the amount and distribution of fine and coarse woody debris,
- site preparation, and
- the conversion of subsurface to surface runoff along roads and skid trails.
The duration of hydrologic change associated with MPB will depend on:
- whether the entire overstory has died or been logged,
- the amount of ground disturbance,
- the presence, age, and density of advance regeneration, and
- the regeneration delay.
At the stand scale, the initial hydrologic
effects of logging are expected to be greater than the initial
effects of beetle kill alone. However, with prompt reforestation it
is possible that the duration of hydrologic change will be reduced
in regenerating clearcuts relative to that in un-salvaged pine
stands. These differences have not been well-quantified and are the
subject of current research, as are the effects of MPB at the larger
watershed scale.
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Hydrologic changes that can result from the MPB and salvage harvesting include:
- increased peak flows and water yield,
- increased surface erosion,
- damage to forest road surfaces, cuts and fills, and drainage structures,
- channel destabilization,
- loss of fish habitat
- increased landslide activity,
- elevated water tables,
- loss of soil and site productivity, and
- loss of water quality.
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To mitigate the effects of the MPB infestation on water and
watersheds, the following recommendations should be considered by
forest resource planners where practicable:
- salvage log in stages by using a variety
of cutting intensities and retention strategies, distributed
over the landscape, to desynchronize runoff,
- avoid sensitive terrain and soil types and
develop erosion control plans where necessary,
- minimize harvesting within riparian areas,
- maintain a diversity of cover types and
minimize post-salvage reforestation delays through single tree
or patch retention to protect advanced regeneration as well as
non-coniferous forest vegetation,
- leave fine and coarse woody debris in
openings where possible to delay surface runoff,
- develop watershed management strategies
that will maintain other forest resource values,
- construct, inspect, and maintain roads to
ensure natural surface and shallow subsurface drainage remain in
tact,
- upgrade drainage networks on permanent
roads prior to salvage logging as necessary to accommodate
expected increases in peak flows, and
- increase inter-agency and public
communication regarding the issues, hazards, and risks in
watersheds affected by MPB beginning with the identification of
watersheds where downstream risks to public safety and
infrastructure could be increased.
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Research projects, both field and modeling, address questions about the
effects of MPB-related stand mortality, salvage logging, partial retention, and
regeneration effects on snow accumulation and melt, stand water balances,
streamflow, channel stability, water quality, and aquatic habitat.
Sources of information
Summaries of post-MPB hydrology:
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A series of
overview maps showing the extent of
pine dominated forest cover in the Northern and Southern Interior
Forest Regions were produced as part of an inter-agency flood hazard
mitigation initiative led by the Provincial Emergency Program. The
objectives of this initiative are:
- “to coordinate government response to flood
consequences resulting from beetle infestation, and
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to reduce risk to communities and provincial
infrastructure from infestation related hazards.”
One of the key tasks set out by the Assistant
Deputy Ministers of the Ministry of Environment, Transportation, and
Forests and Range was to develop a risk assessment framework
including hazard identification.
The maps show all 3rd order and
higher watershed boundaries, communities, and public infrastructure,
the extent of forest consisting of more than 40% lodgepole pine, and
areas logged over the past 25 years within a Forest District. Data
are not currently available for the following areas:
- areas logged and affected by recent wildfires from 2003 on TFLs and some parks
- Peace
- Fort Nelson
- Skeena-Stikine
- Nadina - east of Tweedsmuir Park
- Quesnel - west and east tips
- Central Cariboo – south and central areas
- Chilcotin - large part of southern half as well as northern tip
- 100 Mile house - west
- Headwaters – north-east
- Kamloops - south
- Rocky Mountain – north-west tip
- Arrow Boundary - centre and north
Summary tables listing all third and higher
order watersheds, their area, the area of pine dominated forest, and
the area logged are also provided for each District. The maps and
tables provide a useful indication of the extent of both lodgepole
pine leading forest types and past disturbance in most watersheds
throughout the interior of B.C. They will help to focus attention
on areas where significant stand mortality is expected. These maps
should be used in conjunction with flood risk maps to identify areas
that have a higher level of flood risk in the post-MPB period.
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Contacts for additional forest hydrology
information:
Contacts for map related questions:
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