Abstract. A preliminary field-based investigation was undertaken in a small (< 10 km2) river valley located in the mountainous Jura region of
northwest Switzerland. The aims of the work were to assess sediment
generation and annual sediment transport rates by tree throw on forested
hillslopes and to document surface hydrology characteristics on four fresh
tree throw mounds associated with recent tree throws over a 24 d
monitoring period. For the tree throw mounds, average sediment recovery
ranged from 7.7–28.2 g (dry weight), equivalent to a suspended sediment
concentration of 145.2–327.8 g L−1, and runoff coefficients ranged from
1.0 %–4.2 %. Based on a soil bulk density value of 1044 kg m−3,
upslope runoff generation areas were denuded by an average of 0.14 mm within
the 24 d monitoring period, representing an erosion rate equivalent to 2.1 mm a−1. This means that a ca. 50 cm high tree throw mound could
theoretically persist for around 200–250 years. For tree throw work, the
dimensions of 215 fallen trees were measured and their locations mapped in
12 separate locations where tree throw was prominent along the river valley,
representing a cumulative area equivalent to 5.3 ha (average density equivalent
to 43 trees ha−1). The 215 tree throws generated a total of 20.1 m3
of fine sediment (< 2 mm dia.), or the equivalent of 3.8×10-4 m3 m−2. The process of tree throw was originally attributed to two
extreme weather events that occurred across west and central Europe in late
December 1999. Taking the 18-year period since both storms, this represents
an annual sediment transport rate of 2.7×10-5 m3 m−1 a−1. Exploring the relationship with wind on fall direction, however,
65.5 % of mapped tree throws (n= 143) generally fell in a downslope
direction irrespective of hillslope aspect on which they were located. Given
the similar fall orientation for most trees, this infers that severe storms
may not have been responsible for the majority of tree throws, but instead,
their upheave might be related to root failure. Given the relative maturity
(average age 41 years) of fallen trees in this river valley, our data suggest
that once trees attain a certain age, their physiognomy (i.e. height, mass,
and centre of gravity) compromises their ability to remain securely
anchored. We tentatively attribute this possibility to the presence of
bedrock close to the surface, and to the shallow soil profile overlaying the
steep rocky slopes. More in-depth studies are required to firstly confirm
our findings, and secondly, tree throw studies should be undertaken in other
Jura mountain river valleys to assess whether these results are
representative.
Sediment Load and Suspended Sediment Concentration Prediction
