scholarly journals A Swainson's hawk staging area long the Missouri Coteau in southeast Saskatchewan

Blue Jay ◽  
2005 ◽  
Vol 63 (1) ◽  
Author(s):  
Martin Bailey ◽  
Carol Bjorklund
Keyword(s):  
Missouri Coteau ◽  
Staging Area

Evidence of Brent Geese Branta bernicla Moving between an Autumn Staging Area in East Hokkaido and Wintering Sites in West Hokkaido and Northern Honshu

2020 ◽  
Vol 19 (2) ◽  
pp. 211
Author(s):  
Yusuke Sawa ◽  
Chieko Tamura ◽  
Toshio Ikeuchi ◽  
Tetsuo Shimada ◽  
Kaoru Fujii ◽  
...  
Keyword(s):  
Branta Bernicla ◽  
Staging Area

Optimizing ETL by a Two-Level Data Staging Method

2016 ◽  
Vol 12 (3) ◽  
pp. 32-50
Author(s):  
Xiufeng Liu ◽  
Nadeem Iftikhar ◽  
Huan Huo ◽  
Per Sieverts Nielsen
Keyword(s):  
Data Warehouse ◽  
Data Warehousing ◽  
Data Extraction ◽  
Data Staging ◽  
Staging Area ◽  
Level Data ◽  
Different Types ◽  
Operational Systems ◽  
Early Late ◽  
Central Data

In data warehousing, the data from source systems are populated into a central data warehouse (DW) through extraction, transformation and loading (ETL). The standard ETL approach usually uses sequential jobs to process the data with dependencies, such as dimension and fact data. It is a non-trivial task to process the so-called early-/late-arriving data, which arrive out of order. This paper proposes a two-level data staging area method to optimize ETL. The proposed method is an all-in-one solution that supports processing different types of data from operational systems, including early-/late-arriving data, and fast-/slowly-changing data. The introduced additional staging area decouples loading process from data extraction and transformation, which improves ETL flexibility and minimizes intervention to the data warehouse. This paper evaluates the proposed method empirically, which shows that it is more efficient and less intrusive than the standard ETL method.

scholarly journals JEPAPLOK: KOREOGRAFI PENGGAMBARAN HEWAN MITOLOGI JAWA

JOGED ◽  
2020 ◽  
Vol 16 (2) ◽  
pp. 188-201
Author(s):  
Chorine Nur Shofa
Keyword(s):  
Point Of View ◽  
The Body ◽  
Final Part ◽  
Staging Area ◽  
Basic Motion

Jepaplok merupakan judul dari sebuah karya tari kelompok yang di dalamnya melibatkan sembilan penari perempuan. Kata Jepaplok yaitu berasal dari Njeplak (Manggap) dan Nyaplok (mencaplok). Karya tari ini berawal dari pertunjukan Jaranan di Tulungagung Jawa Timur. Barongan atau biasa disebut Caplokan/Jepaplok adalah penggambaran hewan mitologi berupa ular naga sebagai penguasa hutan yang jahat. Sosok yang dilihat dari segi visualnya menyeramkan dan ganas, serta dari sudut geraknya yang sangat ekspresif. Gerak-gerak dasar yang digunakan antara lain seperti leang-leong, ngaplak, ngepruk, sondongan, pattetan, dan sundangan. Karya tari Jepaplok terdiri dari 4 bagian adegan. Pada bagian introduksi dipertunjukkan sosok Barongan dan Jaranan yang berbeda ruang dan kemudian saling menyerang. Bagian 1 berfokus pada gerak Barongan tanpa menggunakan properti topeng. Pada bagian 2 persiapan penyerangan terhadap penari Jaranan, sehingga dalam bagian ini sudah menggunakan properti topeng. Bagian 3 lebih kepada esensi penggunakan topeng dan diolah dengan permainan ritme dan menggunakan komposisi berpasangan. Bagian 4 yaitu akhir dari pertunjukan karya tari Jepaplok yaitu perangan Barongan dan Jaranan. Tetapi pada bagian akhir ini tidak semata-mata saling berhadapan satu dengan yang lain melainkan hanya sebatas permainan per kelompok. ABSTRACT Jepaplok is the title of a workgroup in which dance involving nine female dancers. The word Jepaplok is derived from Njeplak (Mangap) and Nyaplok (annexed). This dance originated in the works of interest in dance salon when watching a show used Jaranan (dance horse) in Tulungagung, East Java. The point of view of the Director of the dance stopped when one of the characters enter the staging area performance Barongan. Suspenseful atmosphere emerges when section toward the battle between used Horse and Barongan. Barongan or commonly called Caplokan/Jepaplok is the depiction of mythological animals in the form of a dragon serpent as ruler of the evil forest. The figure is seen in terms of the Visual sinister and vicious, as well as from the point of highly expressive movements that inspired the stylist for him to dance in a group dance with paper based on motion and feel the music used Jaranan Sentherewe Tulungagung, East Java. The focus of the implementation work of the dance called Jepaplok is more to perangan and Barongan figures. Basic motion-motion that is used among other things such as leang-leong, ngaplak, ngepruk, sondongan, pattetan, and sundangan. In the work of this Jepaplok dance doesn't bring up the story and consists of four parts of the scene. On the introduction of a dance figure demonstrating Barongan and different spaces used Horse and then each other. Part one is more focused on motion the Barongan poured into members of the body of a dancer without using the mask property. In part two, namely more to preparation which showed Barongan attacks against dancers used Horse, so in this section are already using property mask. Part three more to the essence of the use of mask and mingled with the game rhythm and composition using paired. Part four, namely the ending of the show dance work Jepaplok, as in general the final part of the art used Horse namely perangan and Barongan used Horse. But in the end, it does not solely face each other with one another but rather only as a game between groups.

CONTRIBUTIONS TO THE HOLOCENE PALEOECOLOGY OF WESTCENTRAL CANADA: A LATE-GLACIAL DEPOSIT FROM THE MISSOURI COTEAU

1964 ◽  
Vol 42 (6) ◽  
pp. 677-692 ◽  
Author(s):  
J. C. Ritchie ◽  
Bernard de Vries
Keyword(s):  
Great Plains ◽  
Late Glacial ◽  
Pollen Spectrum ◽  
Pollen Diagram ◽  
Glacial Deposit ◽  
Carbon 14 ◽  
Missouri Coteau ◽  
Plant Assemblages ◽  
Mixed Prairie ◽  
Artemisia Pollen

A buried deposit of limnic sediment was excavated from a site on the Missouri Coteau of Saskatchewan, within the Mixed Prairie section of the Great Plains. Carbon-14 determinations indicate that the section is late-glacial, possibly deposited during an interstadial terminated by the Condie (= Valders?) re-advance. On the basis of the records of about 60 taxa of Tracheophyta and a pollen diagram, the section is characterized by lower, middle, and upper plant assemblages. It is suggested that the lower and upper assemblages, distinguished mainly by a Picea – Shepherdia canadensis – Salix – Artemisia pollen spectrum, indicate the prevalence on mesic sites of a spruce forest. The middle assemblage, having an array of macrofossils and a few microfossils of temperate geographical affinity and a pollen spectrum suggesting relatively less spruce and (or) more herbaceous vegetation, is interpreted in terms of a mixed spruce–poplar forest on mesic sites with shrub and grassland communities on the more xeric habitats. This tripartite division of the section in terms of ecologically concordant plant assemblages suggests an amelioration of environment followed by a deterioration which was probably correlative with the Condie re-advance.

Optimal Staging Area Locations and Material Recycling Strategies for Sustainable Highway Reconstruction

2014 ◽  
Vol 29 (8) ◽  
pp. 559-571 ◽  
Author(s):  
Ryan Smith ◽  
Eric Ferrebee ◽  
Yanfeng Ouyang ◽  
Jeffery Roesler
Keyword(s):  
Material Recycling ◽  
Staging Area

Diet selection of lesser white-fronted geeseAnser erythropusat a spring staging area

Ecography ◽  
2003 ◽  
Vol 26 (6) ◽  
pp. 705-714 ◽  
Author(s):  
Juha Markkola ◽  
Marika Niemelä ◽  
Seppo Rytkönen
Keyword(s):  
Diet Selection ◽  
Staging Area ◽  
Selection Of

scholarly journals Enhancement Techniques for Data Warehouse Staging Area

2013 ◽  
Vol 3 (6) ◽  
pp. 1-19
Author(s):  
Mahmoud El-Wessimy ◽  
Hoda M.O. Mokhtar ◽  
Osman Hegazy
Keyword(s):  
Data Warehouse ◽  
Staging Area

BRYOPHYTE SUBFOSSILS OF A LATE-GLACIAL DEPOSIT FROM THE MISSOURI COTEAU, SASKATCHEWAN

1965 ◽  
Vol 43 (8) ◽  
pp. 947-953 ◽  
Author(s):  
B. de Vries ◽  
C. D. Bird
Keyword(s):  
Boreal Forest ◽  
Higher Plants ◽  
Late Glacial ◽  
Organic Layer ◽  
Middle Zone ◽  
Higher Plant ◽  
Glacial Deposit ◽  
Boreal Species ◽  
The North ◽  
Missouri Coteau

Bryophyte and associated macro-subfossils were recovered from a kettle located in prairie southwest of Moose Jaw in the Missouri Coteau of southern Saskatchewan. The higher plants were discussed in an earlier paper.Three samples taken from the organic layer gave C14 datings ranging from 11,650 ± 150 to 10,270 ± 150 B.P.Sixteen species and one variety of Musci were recovered. Eleven of these were found in the lowermost zone at a depth of 510–450 cm. This zone was composed of bryophytes and higher plants characteristic of a modern Picea forest. Fifteen bryophyte taxa were recovered from the middle zone at a depth of 450–290 cm. The macro-subfossils in this zone are typical of a present-day Populus–Picea forest. No bryophytes were found in the upper layer, 290–280 cm characterized by higher plant macro-subfossils and pollen typical of a modern Picea forest.All bryophytes recovered belong to present-day taxa; however, many of the boreal species are not now found in the region as the southern margin of the boreal forest is now 200 miles to the north.

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