JIBE 发表于 2025-3-28 16:06:28
http://reply.papertrans.cn/99/9810/980905/980905_41.pngItinerant 发表于 2025-3-28 21:02:23
http://reply.papertrans.cn/99/9810/980905/980905_42.png无思维能力 发表于 2025-3-29 02:18:03
http://reply.papertrans.cn/99/9810/980905/980905_43.pngObvious 发表于 2025-3-29 06:51:08
The El Niño / Southern Oscillation and Australian vegetationde with ENSO “events” (i.e. anomalously warm sea surface temperatures in the east equatorial Pacific), and for extensive wet periods to accompany “anti-ENSO” events, is well documented. Also well-known is the partial predictability of Australian rainfall anomalies provided by ENSO..Some other ENSO-rCommon-Migraine 发表于 2025-3-29 09:40:18
http://reply.papertrans.cn/99/9810/980905/980905_45.png1分开 发表于 2025-3-29 14:41:10
Towards a better model of the effect of prostrate vegetation cover on wind erosiontubble) model was evaluated against field wind tunnel results from far south-west N.S.W. Fryrear’s equation over estimated the soil loss compared to field wind tunnel results..Fryrear’s model failed to provide meaningful results at low cover levels with the soil loss ratio, . > 1 for percent soil co不知疲倦 发表于 2025-3-29 18:54:20
http://reply.papertrans.cn/99/9810/980905/980905_47.png里程碑 发表于 2025-3-29 23:32:01
Sources and sinks of greenhouse gases in the soil-plant environmentee have significant sources in the soilplant environment and principal sinks in the atmosphere or the oceans. The emphasis is on methodological problems associated with measuring source and sink strengths, but the biogeochemistry of individual gases and problems of scaling to longer times and largerFigate 发表于 2025-3-30 00:12:46
http://reply.papertrans.cn/99/9810/980905/980905_49.png尊严 发表于 2025-3-30 05:23:58
Vegetation-atmosphere interaction in homogeneous and heterogeneous terrain: some implications of mixary discussion, processes at canopy scale are reviewed briefly by outlining two classes of model: comprehensive, multilayer Canopy-Atmosphere Models (CAMs) which attempt to include all physical and biological processes influencing the canopy microclimate and atmospheric exchanges, and single-layer S