https://nova.newcastle.edu.au/vital/access/ /manager/Index en-au 5 Local perceptions of and adaptation to climate variability and change: the case of shrimp farming communitiesin the coastal region of Bangladesh https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:26898 Wed 11 Apr 2018 12:23:56 AEST ]]> Stratification response of soil water content during rainfall events under different rainfall patterns https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:41374 Tue 02 Aug 2022 15:27:25 AEST ]]> East coast low storms and the Pasha Bulker storm - lessons learned five years on https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:25758 Thu 20 Oct 2022 09:48:35 AEDT ]]> The variability of "nature's limit" in South Australia https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:18706 Thu 20 Oct 2022 09:48:22 AEDT ]]> Developing hazard lines in response to coastal flooding and sea level change https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:20497 Sat 24 Mar 2018 07:59:04 AEDT ]]> Spatial analysis of Australian seasonal rainfall anomalies and their relation to east coast lows on the Eastern-Seaboard https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:26488 Sat 24 Mar 2018 07:35:35 AEDT ]]> Testing the statistics of dynamically downscaled rainfall data for the east coast of NSW https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:26490 Sat 24 Mar 2018 07:35:34 AEDT ]]> Use of NARCliM rainfall data for simulating streamflow in the Williams River catchment https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:26433 Sat 24 Mar 2018 07:27:29 AEDT ]]> Explaining changes in rainfall–runoff relationships during and after Australia's Millennium Drought: a community perspective https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:53054 Fri 17 Nov 2023 11:50:47 AEDT ]]> How and to what extent does precipitation on multi-temporal scales and soil moisture at different depths determine carbon flux responses in a water-limited grassland ecosystem? https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:32976 eco), and net ecosystem exchange of CO₂ (NEE). Interestingly, carbon flux showed no relationship with diurnal PRE or phenological-related PRE (precipitation in the growing season and non-growing season). However, carbon flux was significantly related to monthly PRE and to seasonal PRE (spring + summer, autumn). The GPP, Reco, and NEE increased in spring and summer but decreased in autumn with increasing precipitation due to the combined effect of salinization in autumn. The GPP, Reco, and NEE were more responsive to SMC at 0-20 cm depth than at deeper depths due to the shorter roots of herbaceous vegetation. The NEE increased with increasing monthly PRE because soil microbes responded more quickly than plants. The NEE significantly decreased with increasing SMC in shallow surface due to a hysteresis effect on water transport. The results of our study highlight the complex processes that determine how and to what extent PRE at multi-temporal scale and SMC at different depths affect the carbon flux response in a water-limited grassland.]]> Fri 17 Aug 2018 12:20:48 AEST ]]>