Sustainable forest management and impacts on forest responses to a changing climate

Impacts from human activities at varying scales and intensities have a profound influence on forest carbon dynamics in addition to interactions with climate. As such, forest carbon stocks and fluxes are among the least well-defined elements of the global carbon cycle, and great uncertainty remains in predicting the effect of climate change on forest dynamics. In some cases, these management-climate interactions are well known, but often represent a fundamental gap in our understanding of ecosystem responses and are likely to be important in improving modeling of climate change, and in valuing forest carbon. To improve understanding of human induced forest management-climate interactions, a network of permanent study plots has been established in five sites around the world - in the US, UK, Brazil, India and China. The sites are near larger global monitoring (Smithsonian CTFS) plots to facilitate comparisons. At each site, a series of 1-ha plots have been placed in forest stands with differing management regimes and histories. Utilizing citizen scientists from HSBC bank, all trees >5 cm dbh are tagged, mapped, identified to species, and diameter is recorded within each plot. A subset of trees have dendrometer bands attached, to record seasonal growth. Dead wood and litterfall samples are taken, and microclimate is recorded with automatic sensors. Serial measurements will allow correlation of forest dynamics with weather. Although the studies are at an early stage current results indicate above-ground biomass estimates are 102-288 Mg ha-1 for intermediate and mature Liriodendron tulipifera-dominated stands in the US, respectively. In India, mature semi-natural evergreen forests biomass estimates are 192-235 Mg ha-1 while plantation and semi-natural core forests in the UK are estimated at 211-292 Mg ha-1. Successional Atlantic forests in Brazil are estimated to contain 192-235 Mg ha-1. In the US, initial results have demonstrated dramatic differences in microclimate (soil and air temperature and penetrance of phosynthetically active radiation) and canopy structure (the vertical distribution of surfaces) between the intact and selectively logged stands. These variables will be used as indicators of the strength and speed of ecosystem recovery to logging. In the UK, plantations had greater biomass than the semi-natural plots, due to differences in age structure; however, trees above 50 cm dbh comprised 3% of total stems but almost 50% of the biomass in the semi-natural plots. Comparisons will be made among the various modes of forest disturbance to determine how these could influence ecosystem responses to climate change. Increasing human and climatic pressures on the world's forests will necessitate further long-term studies and cross-ecosystem comparisons of this nature which lends itself to application of an intensive citizen science program.