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- W3016033921 abstract "Depth to water table is a simple, commonly used measure of hydrological function in raised bogs. The maximum depth of the water table or the average annual water table is often monitored over the long term to track the hydrological trajectory of the ecosystem. These measures, however, may not take into account the duration of the moisture deficit period. The annual water table moisture deficit (WTMD) at 67 sites in a single disturbed raised bog was calculated using the amount of time that the water table was at each depth below the surface during the moisture deficit season. The calculated value estimates a linearly developing deficit that dewaters the acrotelm during the moisture deficit season. At each site, plant species composition was assigned to one of eight plant community types. The approximate threshold above which bog plant communities will begin transitioning into drier types with taller shrubs and trees was a WTMD of 62 m-days. An annual climatic moisture deficit (CMD) was calculated using daily air temperature, spatially interpolated precipitation and estimated potential evapotranspiration for each site. Mixed-effects modelling of WTMD as a function CMD indicated a positive linear relation for most vegetation types, which was affected by the presence of drainage ditches, ditch blocking, fire and evapotranspiration by shrubs and trees. Tracking the WTMD and its relation to CMD may be useful for assessing ecosystem health and serve as a basis for estimating moisture deficit thresholds for bogs of conservation concern." @default.
- W3016033921 created "2020-04-17" @default.
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- W3016033921 date "2020-04-13" @default.
- W3016033921 modified "2023-09-28" @default.
- W3016033921 title "Plant community type is an indicator of the seasonal moisture deficit in a disturbed raised bog" @default.
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- W3016033921 doi "https://doi.org/10.1002/eco.2209" @default.
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