A narrative of the adventures and escape of Moses Roper : from American slavery /

"Twenty-fourth thousand."

The influence of climate variability on hydrological processes and surface and groundwater hydrochemistry : the tropical upper roper river catchment, Northern Territory, Australia

The Upper Roper River is one of the Australia’s unique tropical rivers which have been largely untouched by development. The Upper Roper River catchment comprises the sub-catchments of the Waterhouse River and Roper Creek, the two tributaries of the Roper River. There is a complex geological setting with different aquifer types. In this seasonal system, close interaction between surface water and groundwater contributes to both streamflow and sustaining ecosystems. The interaction is highly variable between seasons. A conceptual hydrogeological model was developed to investigate the different hydrological processes and geochemical parameters, and determine the baseline characteristics of water resources of this pristine catchment. In the catchment, long term average rainfall is around 850 mm and is summer dominant which significantly influences the total hydrological system. The difference between seasons is pronounced, with high rainfall up to 600 mm/month in the wet season, and negligible rainfall in the dry season. Canopy interception significantly reduces the amount of effective rainfall because of the native vegetation cover in the pristine catchment. Evaporation exceeds rainfall the majority of the year. Due to elevated evaporation and high temperature in the tropics, at least 600 mm of annual rainfall is required to generate potential recharge. Analysis of 120 years of rainfall data trend helped define “wet” and “dry periods”: decreasing trend corresponds to dry periods, and increasing trend to wet periods. The period from 1900 to 1970 was considered as Dry period 1, when there were years with no effective rainfall, and if there was, the intensity of rainfall was around 300 mm. The period 1970 – 1985 was identified as the Wet period 2, when positive effective rainfall occurred in almost every year, and the intensity reached up to 700 mm. The period 1985 – 1995 was the Dry period 2, with similar characteristics as Dry period 1. Finally, the last decade was the Wet period 2, with effective rainfall intensity up to 800 mm. This variability in rainfall over decades increased/decreased recharge and discharge, improving/reducing surface water and groundwater quantity and quality in different wet and dry periods. The stream discharge follows the rainfall pattern. In the wet season, the aquifer is replenished, groundwater levels and groundwater discharge are high, and surface runoff is the dominant component of streamflow. Waterhouse River contributes two thirds and Roper Creek one third to Roper River flow. As the dry season progresses, surface runoff depletes, and groundwater becomes the main component of stream flow. Flow in Waterhouse River is negligible, the Roper Creek dries up, but the Roper River maintains its flow throughout the year. This is due to the groundwater and spring discharge from the highly permeable Tindall Limestone and tufa aquifers. Rainfall seasonality and lithology of both the catchment and aquifers are shown to influence water chemistry. In the wet season, dilution of water bodies by rainwater is the main process. In the dry season, when groundwater provides baseflow to the streams, their chemical composition reflects lithology of the aquifers, in particular the karstic areas. Water chemistry distinguishes four types of aquifer materials described as alluvium, sandstone, limestone and tufa. Surface water in the headwaters of the Waterhouse River, the Roper Creek and their tributaries are freshwater, and reflect the alluvium and sandstone aquifers. At and downstream of the confluence of the Roper River, river water chemistry indicates the influence of rainfall dilution in the wet season, and the signature of the Tindall Limestone and tufa aquifers in the dry. Rainbow Spring on the Waterhouse River and Bitter Spring on the Little Roper River (known as Roper Creek at the headwaters) discharge from the Tindall Limestone. Botanic Walk Spring and Fig Tree Spring discharge into the Roper River from tufa. The source of water was defined based on water chemical composition of the springs, surface and groundwater. The mechanisms controlling surface water chemistry were examined to define the dominance of precipitation, evaporation or rock weathering on the water chemical composition. Simple water balance models for the catchment have been developed. The important aspects to be considered in water resource planning of this total system are the naturally high salinity in the region, especially the downstream sections, and how unpredictable climate variation may impact on the natural seasonal variability of water volumes and surface-subsurface interaction.

Two couples including Willy Tese Moses and Gertrud Moses walking down a street; Bad Ragaz, Switzerland Portraits Couples

Digital Image

Willy Tese Moses and others seated at an outdoor table; Chile Portraits Groups

Digital Image

Eyeglasses of Moses Mendelssohn.

Digital Image

Edna and Moses Stern with daughters Erna and Annie Portraits Family

Grandparents of Margot Gerson

goldschmidt, max; goldschmidt lotte; goldschmidt fritz; goldschmidt frieda; heilbrunn lotte; goldscmidt anna; simon moses Portraits Family

Digital Image

Sir Moses Montefiore Commemorative Medal

Obverse: Portraits of Sir Moses Montefiore and Judith Montefiore. Reverse: The house of Mishkenot Shaanim, in the background the windmill of Yemin Moshe in Jerusalem.

Moses Kligsberg 1930s-1974

The papers relate to Kligsberg's scholarly interests and to his work at YIVO. Included are: Manuscripts relating to topics in Jewish sociology, psychology. Kligsberg's survey of the autobiographies of Jewish youth in Poland gathered by YIVO in the 1930s for a contest. Materials relating to the *YIVO News*, YIVO radio programs, YIVO contests. Materials relating to the collection of archival materials for the YIVO Archives. Materials on the Bund. Papers of Herman Kruk, librarian, archivist and diarist in the Vilna Ghetto. Records of the United Jewish Survivors of Nazi Persecutions, 1946-1957.

Letter from Manuel Josephson to Moses Seixas, February 4, 1890

Digital image

Letter to K.K.S.I. from Moses and Simon Content, August 19, 1828

Digital image

Letter from Abraham Touro to Moses B. Seixas

Digital image

Resolution of K.K.S.I. to Sir Moses Montefiore regarding his visit to Russia

Digital image