An Eruv for St Ives? Religion,identity, place and conflict on the Sydney north shore     

John Connell  Kurt Iveson 《The Australian geographer》2014,45(4):429-446

Religious identity, when marked by physical changes to urban landscapes, has been a cause of tension and conflict in many cities. In the Sydney suburb of St Ives, an attempt to create an eruv, a symbolic and only partly physical boundary around orthodox Jewish space, was vigorously opposed and eventually defeated through the planning system. The religious and physical significance of the eruv resulted in diverse rationales of opposition, centred on the physical and environmental impact, the conceptual nature of boundaries and the role of religion and ‘modernity’ in everyday suburban life. The place of an eruv was opposed with reference to spatial imaginaries of the nation, the suburb and the secular public, as religion and worship intersected with the politics of urban citizenship and belonging. Each of these spatial imaginaries was constructed by opponents in such a way as to deny a place for an eruv in St Ives, and reinforced through the application of planning instruments which eventually refused permission for an eruv. To many residents, public space was seen to be at risk, raising complex questions over amenity, the politics and perception of difference and what is in or out of place. The planning framework adjudicating such development proposals must transcend such imaginaries in the production of public spaces in multicultural cities.  相似文献   

The largest floods in the High Rhine basin since 1268 assessed from documentary and instrumental evidence     

Oliver Wetter  Christian Pfister  Rolf Weingartner  Jürg Luterbacher  Tom Reist  Jürg Trösch 《水文科学杂志》2013,58(5):733-758

Abstract

The magnitudes of the largest known floods of the River Rhine in Basel since 1268 were assessed using a hydraulic model drawing on a set of pre-instrumental evidence and daily hydrological measurements from 1808. The pre-instrumental evidence, consisting of flood marks and documentary data describing extreme events with the customary reference to specific landmarks, was “calibrated” by comparing it with the instrumental series for the overlapping period between the two categories of evidence (1808–1900). Summer (JJA) floods were particularly frequent in the century between 1651–1750, when precipitation was also high. Severe winter (DJF) floods have not occurred since the late 19th century despite a significant increase in winter precipitation. Six catastrophic events involving a runoff greater than 6000 m ³ s^‐1 are documented prior to 1700. They were initiated by spells of torrential rainfall of up to 72 h (1480 event) and preceded by long periods of substantial precipitation that saturated the soils, and/or by abundant snowmelt. All except two (1999 and 2007) of the 43 identified severe events (SEs: defined as having runoff > 5000 and < 6000 m ³ s ^‐1) occurred prior to 1877. Not a single SE is documented from 1877 to 1998. The intermediate 121-year-long “flood disaster gap” is unique over the period since 1268. The effect of river regulations (1714 for the River Kander; 1877 for the River Aare) and the building of reservoirs in the 20th century upon peak runoff were investigated using a one-dimensional hydraulic flood-routing model. Results show that anthropogenic effects only partially account for the “flood disaster gap” suggesting that variations in climate should also be taken into account in explaining these features.

Citation Wetter, O., Pfister, C., Weingartner, R., Luterbacher, J., Reist, T., & Trösch, J. (2011) The largest floods in the High Rhine basin since 1268 assessed from documentary and instrumental evidence. Hydrol. Sci. J. 56(5), 733–758.  相似文献   

Suspended silt and salinity tolerances of the first zoeal stage of the fiddler crab Uca annulipes (Decapoda: Brachyura) and why marine connectivity is essential to the survival of the species     

N Peer  NAF Miranda  R Perissinotto 《African Journal of Marine Science》2016,38(2):161-169

Fiddler crabs (Uca spp.) undergo the zoeal stage of development in open-ocean waters, where they experience stable salinity levels, low turbidity and reduced predation. The St Lucia estuarine system has undergone many geomorphological changes, both natural and anthropogenic, and the estuary mouth has been closed since the early 2000s. Despite recent attempts to improve marine connectivity, it remains limited, occurring primarily on the flood tide through channels connected to the adjacent Mfolozi River. Larval export from the St Lucia Estuary is therefore almost non-existent. A laboratory study was undertaken to examine the silt and salinity tolerance of Uca annulipes first stage zoeae, to investigate whether survival in the closed-estuary conditions would be possible. Salinity tolerance was narrow, with zoeae displaying 100% mortality at salinities <20 and >35 after five days. Zoeae were widely tolerant to silt loading and did not display a significant decrease in survival over a range of 0–1 000 NTU. A limited salinity tolerance is in accordance with the life-history strategy of fiddler crabs, and a high tolerance to turbid waters can be advantageous to small-bodied merozooplankton. Given the stenohaline nature of the zoeae, marine connectivity is therefore essential for the persistence of U. annulipes in this estuarine habitat.  相似文献   

Coral bleaching indices and thresholds for the Florida Reef Tract, Bahamas, and St. Croix, US Virgin Islands   总被引：2，自引：0，他引：2  

Manzello DP  Berkelmans R  Hendee JC 《Marine pollution bulletin》2007,54(12):1923-1931

It is well established that elevated sea temperatures cause widespread coral bleaching, yet confusion lingers as to what facet of extreme temperatures is most important. Utilizing long-term in situ datasets, we calculated nine thermal stress indices and tested their effectiveness at segregating bleaching years a posteriori for multiple reefs on the Florida Reef Tract. The indices examined represent three aspects of thermal stress: (1) short-term, acute temperature stress; (2) cumulative temperature stress; and (3) temperature variability. Maximum monthly sea surface temperature (SST) and the number of days >30.5 °C were the most significant; indicating that cumulative exposure to temperature extremes characterized bleaching years. Bleaching thresholds were warmer for Florida than the Bahamas and St. Croix, US Virgin Islands reflecting differences in seasonal maximum SST. Hind-casts showed that monthly mean SST above a local threshold explained all bleaching years in Florida, the Bahamas, and US Virgin Islands.  相似文献