First CRDS-measurements of water vapour continuum in the 940nm absorption band

Measurements of near-infrared water vapour continuum using continuous wave cavity ring down spectroscopy (cw- CRDS) have been performed at around 10611.6 and 10685:2 cm1. The continuum absorption coefficients for N2- broadening have been determined for two temperatures and wavenumbers. These results represent the first near-IR continuum laboratory data determined within the complex spectral environment in the 940nm water vapour band and are in reasonable agreement with simulations using the semiempirical CKD formulation.

Comparisons between the in vitro and in vivo efficacies of potential fungal antagonists of Armillaria mellea

Seventeen fungal isolates were tested in vitro as potential antagonists of two isolates of the root rot pathogen, Armillaria mellea. Some of the isolates were also added on mushroom composts with living mycelia to the roots of Armillaria-inoculated potted strawberry plants in the glasshouse to find out if they had the same degree of efficacy against the disease. Dactylium dendroides isolate SP was the most effective in reducing mycelial growth of A. mellea isolate 1 (Am1), followed by Trichoderma harzianum isolate Th2 and T. viride isolate Tv4. Th2, Th22, Tv3 and SP grew extensively over Am1 colonies, disintegrating the rhizomorphs. Isolate Tham1 of T hamatum was the most effective in reducing mycelial growth of A. mellea isolate 2 (Am2), followed by Tv3. Th12, Th22, Tv1, Tv3 and SP inhibited the initiation and growth of rhizomorphs of Am2. Regeneration tests showed that both Am1 and Am2 attacked by Trichoderma isolates and SP were no longer viable. Th23 and SP were almost as effective in vivo as in vitro. But isolate Co of Chaetomium olivaceum, which was ineffective in vitro, was found effective in vivo. Conversely, Th2, which exhibited good antagonistic activity in vitro, performed poorly in vivo. These results show that the in vitro and in vivo efficacies of potential antagonists may not necessarily be closely correlated. Hence, there is a danger that potentially effective isolates may be discarded if decisions are made only on the basis of preliminary screening tests carried out under laboratory conditions.

Calculations of rovibrational energies and dipole transition intensities for polyatomic molecules using MULTIMODE

We report rigorous calculations of rovibrational energies and dipole transition intensities for three molecules using a new version of the code MULTIMODE. The key features of this code which permit, for the first time, such calculations for moderately sized but otherwise general polyatomic molecules are briefly described. Calculations for the triatomic molecule BF(2) are done to validate the code. New calculations for H(2)CO and H(2)CS are reported; these make use of semiempirical potentials but ab initio dipole moment surfaces. The new dipole surface for H(2)CO is a full-dimensional fit to the dipole moment obtained with the coupled-cluster with single and double excitations and a perturbative treatment of triple excitations method with the augmented correlation consistent triple zeta basis set. Detailed comparisons are made with experimental results from a fit to relative data for H(2)CS and absolute intensities from the HITRAN database for H(2)CO.

Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts?

Confidence in projections of global-mean sea level rise (GMSLR) depends on an ability to account for GMSLR during the twentieth century. There are contributions from ocean thermal expansion, mass loss from glaciers and ice sheets, groundwater extraction, and reservoir impoundment. Progress has been made toward solving the “enigma” of twentieth-century GMSLR, which is that the observed GMSLR has previously been found to exceed the sum of estimated contributions, especially for the earlier decades. The authors propose the following: thermal expansion simulated by climate models may previously have been underestimated because of their not including volcanic forcing in their control state; the rate of glacier mass loss was larger than previously estimated and was not smaller in the first half than in the second half of the century; the Greenland ice sheet could have made a positive contribution throughout the century; and groundwater depletion and reservoir impoundment, which are of opposite sign, may have been approximately equal in magnitude. It is possible to reconstruct the time series of GMSLR from the quantified contributions, apart from a constant residual term, which is small enough to be explained as a long-term contribution from the Antarctic ice sheet. The reconstructions account for the observation that the rate of GMSLR was not much larger during the last 50 years than during the twentieth century as a whole, despite the increasing anthropogenic forcing. Semiempirical methods for projecting GMSLR depend on the existence of a relationship between global climate change and the rate of GMSLR, but the implication of the authors' closure of the budget is that such a relationship is weak or absent during the twentieth century.