In this study nine new species and a new genus of Brachodidae are described from tropical Asia and Papua New Guinea. Synechodes polias sp. nov. and Synechodes tamila sp. nov. are described from Sulawesi and southern India, respectively. A new genus, Saccocera gen. nov. (type species Miscera orpheus Kallies, 2004), is described to accommodate five species occurring from Taiwan and Sumatra across Melanesia to Papua New Guinea. It differs significantly from the related genera Miscera Walker, 1863 and Synechodes Turner, 1913 in morphological details of the head and the male and female genitalia. Two species of Saccocera are described here, Saccocera panaras sp. nov. from Papua New Guinea and Saccocera miangkabau sp. nov. from Sumatra. Furthermore, Miscera minahasa sp. nov. and Paranigilgia mariannae sp. nov. are described from Sulawesi, Paranigilgia brandti sp. nov. and Nigilgia atribractea sp. nov. from Papua, and Nigilgia browni sp. nov. is described from Christmas Island. Finally, Synechodes heppneri Kallies, 1998 syn. nov. is reverted to a junior synonym of Synechodes coniophora Turner, 1913. Nigilgia anactis Diakonoff, 1982 is figured for the first time and its distribution in Asia is discussed.
Wild, M.; Ohmura, A.; Feichter, J.; Stier, P.; Robock, A.; Li, H.
Recent evidence suggests that the amount of solar radiation reaching the earth surface is not stable over time but exhibits significant decadal variations. These variations, in addition to the changes in thermal radiation induced by alterations in greenhouse gases, cause changes in radiative forcings which may significantly affect surface climate. Observations from the Global Energy Balanced Archive (GEBA) and Baseline Surface Radiation Network (BSRN) databases at the Swiss Federal Institute of Technology suggest that surface solar radiation, after decades of dimming, reversed into a brightening since the mid 1980s at widespread locations. These changes are in line with a recovery of atmospheric transparency, possibly related to reduced aerosol loadings due to air pollution control and the breakdown of industry in formerly Communist countries. Not many GCMs currently represent aerosol effects with a degree of sophistication to capture such effects, but we used a special version of the Max Planck Institute for Meteorology GCM which includes a detailed aerosol scheme, ECHAM5-HAM, to investigate the observed trends. In addition, we investigate the potential impact of the variations in surface radiation on other elements of the climate system, such as soil moisture, which shows changes in line with the changes in radiation. Reference: Wild, M., Gilgen, H., Roesch, A., Ohmura, A., Long, C., Dutton, E., Forgan, B., Kallis, A., Russak, V., Tsvetkov, A., 2005: From dimming to brightening: Decadal changes in solar radiation at the Earth's surface. Science , 308, 847-850
de Beer, K. J.; Hoffman, M. J.
Dr M.J. Hoffman, Head of the Department Physics, University of the Free State (UFS), presented a paper at the Duineveld Secondary School in Upington, to enhance the idea of a natural observatory centre in the Northern Cape. Quite aptly, the National Institute for Higher Education: Northern Cape (NIHE) also invited a renowned African astronomer, Dr T Medupe, to address their graduation ceremony in 2005. However, Dr Albert Strydom, Programme Head of Tourism Management at the Central University for Technology, Free State (CUT), is very much aware of the delicate nature of this type of high scientific profile in Tourism Management. It is foreseen by Dr Kallie de Beer, Director of Distance Education, that teaching and learning in this field will predominantly be conducted via Open and Distance e-Learning (ODeL). Consequently, it is also important to understand the philosophy of ODeL within global and Africanized perspectives. Astronomy, in this case, offers excellent examples of Africanised science in practice to add scientific value to tourist packages in the Northern Cape. (www.saao.ac.za/assa/aahs).
Mercado, L.; Bellouin, N.; Sitch, S.; Boucher, O.; Huntingford, C.; Wild, M.; Cox, P. M.
photosynthesis for climate model applications. Tellus Series B-Chemical and Physical Meteorology, 59, 553-565. Niyogi D., Chang H.I., Saxena V.K., Holt T., Alapaty K., Booker F., Chen F., Davis K.J., Holben B., Matsui T., Meyers T., Oechel W.C., Pielke R.A., Wells R., Wilson K. & Xue Y.K. (2004) Direct observations of the effects of aerosol loading on net ecosystem CO2 exchanges over different landscapes. Geophysical Research Letters, 31. Oliveira P.H.F., Artaxo P., Pires C., De Lucca S., Procopio A., Holben B., Schafer J., Cardoso L.F., Wofsy S.C. & Rocha H.R. (2007) The effects of biomass burning aerosols and clouds on the CO2 flux in Amazonia. Tellus Series B-Chemical and Physical Meteorology, 59, 338-349. Roderick M.L., Farquhar G.D., Berry S.L. & Noble I.R. (2001) On the direct effect of clouds and atmospheric particles on the productivity and structure of vegetation. Oecologia, 129, 21-30. Stanhill G. & Cohen S. (2001) Global dimming: a review of the evidence for a widespread and significant reduction in global radiation with discussion of its probable causes and possible agricultural consequences. 107, 255-278. Wild M., Gilgen H., Roesch A., Ohmura A., Long C.N., Dutton E.G., Forgan B., Kallis A., Russak V. & Tsvetkov A. (2005) From dimming to brightening: Decadal changes in solar radiation at Earth's surface. Science, 308, 847-850.
recent absence of solar dimming may have allowed the greenhouse effect to finally develop at full size, as seen in accelerated temperature increases in the 1990s. The rate of temperature change at land surfaces has increased by an order of magnitude in the period 1985-2002 where solar dimming was absent, compared to the period with significant dimming (1958-1985). In the 1990s, more energy may therefore have been available at the surface compared to earlier decades, favoring, for example, an accelerated retreat of worldwide glaciers, or higher evaporation in areas of unlimited water supply and associated reduced soil moisture tendencies, with associated implications for the global hydrological cycle. Reference: Wild, M., Gilgen, H., Roesch, A., Ohmura, A., Long, C., Dutton, E., Forgan, B., Kallis, A., Russak, V., Tsvetkov, A., 2005: From dimming to brightening: Decadal changes in solar radiation at the Earth's surface. Science , 308, 847-850.
Jones, Julian D. C.; Tatam, Ralph P.
fibre optic gyroscope, conventionally taken to date from the first experimental demonstration by V Vali and R W Shorthill (1976 'Fibre ring interferometer' Appl. Opt. 15 1099-100). It is an indication of the health of the community that the successful maturity of some applications is complemented by the new technologies that will be the basis of the future development of the field, and here the content of this special issue is an interesting indication of likely areas of growth. Essentially all current fibre optic systems are based on solid, doped fused silica fibres, which are the basis of the world's telecommunications industry. However, over the last decade an exciting development has been micro-structured fibres, whose waveguiding properties owe as much to the structure of the fibre as to the materials from which they are made. The significance for sensing applications is considerable, with opportunities to achieve properties for dispersion, environmental sensitivity, wavelength range and power-handling quite different from the capabilities of conventional fibre. Thus it is not surprising that several of the papers in the issue (by Cordeiro, Martynkien, Bock, Wolinski, Michie, Digonnet and Kilic) are devoted to applications of such fibres—photonic crystal fibres (PCF), as they are often called. Digonnet's contribution is especially interesting, being concerned with the use of hollow-core photonic bandgap fibre to form a gyroscope, hence avoiding the many subtle non-linear optical effects that can degrade the performance of a conventional fibre gyroscope. PCF are not the only special fibres to feature in the issue: polymer fibres are of increasing interest for sensing applications (O'Keeffe, Kiesel, Kalli and Ashley), not least for their ability to withstand high levels of strain. In-fibre gratings continue to be a very important area in the field, and are well represented in the issue (Ni, González-Segura, Chen, Falate, Kamikawachi, Wang and Correia). We hope
Sellami, Haykel; Benabdallah, Sihem; La Jeunesse, Isabelle; Herrmann, Frank; Vanclooster, Marnik
. López-Moreno, J. I., Vicente-Serrano, S. M., Moran-Tejeda, E., Zabalza, J., Lorenzo-Lacruz, J., and García-Ruiz, J. M.: Impact of climate evolution and land use changes on water yield in the ebro basin, Hydrology and Earth System Sciences, 15, 311-322, 10.5194/hess-15-311-2011, 2011. Ludwig, R., Roson, R., Zografos, C., Kallis. Towards an inter-disciplinary research agenda on climate change, water and security in southern Europe and neighbouring countries. Environ. Sci. Policy. 14: 794-803, 10.1016/j.envsci.2011.04.003, 2011. Richter, B. D., Baumgartner, J.V., Powell, J., Braun, D. P.: Method for Assessing Hydrologic Alteration within Ecosystems, Conservation Biology, 10, 11, 1996. Schneider, C., Laizé, C. L. R., Acreman, M. C., and Flörke, M.: How will climate change modify river flow regimes in Europe? Hydrology and Earth System Sciences, 17, 325-339, 10.5194/hess-17-325-2013, 2013.
Tanaka, Katsumasa; Imamovic, Adel; Folini, Doris; Ohmura, Atsumu; Wild, Martin
Industrial Era. Journal of Climate, 20, 4874-4883. Ohmura A (2009) Observed decadal variations in surface solar radiation and their causes. Journal of Geophysical Research, 114, D00D05. Ohmura A, Lang H (1989) Secular variation of global radiation over Europe. In: Lenoble J, Geleyn JF, Deepak A (eds) Current Problems in Atmospheric Radiation. Hampton, pp 98-301. Shepherd JM (2005) A Review of Current Investigations of Urban-Induced Rainfall and Recommendations for the Future. Earth Interactions, 9, 1-27. Skeie RB, Berntsen TK, Myhre G, Tanaka K, Kvalevåg MM, Hoyle CR (2011) Anthropogenic radiative forcing time series from pre-industrial times until 2010. Atmospheric Chemistry and Physics, 11, 11827-11857. Wild M (2009) Global dimming and brightening: A review. Journal of Geophysical Research, 114, D00D16. Wild M, Gilgen H, Roesch A, Ohmura A, Long CN, Dutton EG, Forgan B, Kallis A, Russak V, Tsvetkov A (2005) From Dimming to Brightening: Decadal Changes in Solar Radiation at Earth's Surface. Science, 308, 847-850.