6 Planungskunst für eine resiliente Stadt-Land- Region

2021 ◽  
pp. 229-266
Keyword(s):  
1995 ◽  
Vol 165 ◽  
pp. 53-58
Author(s):  
N Henriksen

The second field season of the Geological Survey of Greenland's (GGU) mapping project in eastern North Greenland (1993–95) was carried out according to plan and with full accomplishment of all geoscientific goals. The programme aims at producing a general overview of the onshore geology of the Jokelbugten to Kronprins Christian Land region (78–81 °N) in eastern North Greenland (Fig. 1) to be compiled as sheet no. 9 in GGU's 1:500 000 geological map sheet series; this is the last remaining incomplete map sheet at this scale in North and North-East Greenland. The field work was initiated in 1993 with limited reconnaissance work (Henriksen, 1994a), and in 1994 the first of two more intensive field campaigns was carried out. In addition to establishing a general overview of the regional geology the work aims at obtaining an evaluation of the economic geological potential of the region, in respect of both minerals and hydrocarbons. Two glaciological programmes were fully integrated with the project: one was carried out by the Alfred Wegener Institute (AWi), Bremerhaven, Germany, while the other was partly based on a special grant from the Nordic Council of Ministers.


Author(s):  
Hop Vinh Dao ◽  
Tuyet Thi Anh Vo

In the circumstance of the Chinesse emigrants going abroad to seek shelter and find new lands, especially southeast Asia, Dang Trong of Dai Viet kingdom has gradually become a point of arrival which attracts them strongly. Depending on geographic position of contigous sea and advantage of Dang Trong context at home and abroad, Chinese merchants and emigrants have come to the central coastal parts (especially in Quang Nam, Quang Ngai, Binh Dinh, and Phu Yen). Having settled in southeast Asia region as well as in the central part of Vietnam, Chinese emigrants have preseved their traditional culture to gain achievements in this land region. Besides, they have actively integrated into native communities, exchanging culture for prosperity and development. This paper indicates cultural exchanges, integration and development of the Hoa in the central coastal provinces in history and present, which asserts their contributions in the fields of culture, economy and society to build Vietnam nation, notably in the age of present international integration.


1974 ◽  
Vol 109 ◽  
pp. 1-51
Author(s):  
K Perch-Nielsen ◽  
K Birkenmajer ◽  
T Birkelund ◽  
M Aellen

A revised stratigraphic scheme is presented for the Triassic rocks between Kong Oscars Fjord and Scoresby Sund, East Greenland. The Triassic succession is described as the Scoresby Land Group comprising four formations. The lower two formations (Wordie Creek Formation and Pingo Dal Formation) belong to the Nordenskiöld Bjerg Subgroup, while the upper two formations (Gipsdalen Formation and Fleming Fjord Formation) belong to the Kap Biot Subgroup. The total thickness of the Triassic sequence attains 1000 to 1500 m of which less than half is composed of marine sediments. The remainder consists of continental deposits and includes red-beds with an important evaporite complex in the middle of the succession.


2009 ◽  
Vol 10 (4) ◽  
pp. 1026-1039 ◽  
Author(s):  
Benjamin R. Lintner ◽  
J. David Neelin

Abstract An idealized prototype for the location of the margins of tropical land region convection zones is extended to incorporate the effects of soil moisture and associated evaporation. The effect of evaporation, integrated over the inflow trajectory into the convection zone, is realized nonlocally where the atmosphere becomes favorable to deep convection. This integrated effect produces “hot spots” of land surface–atmosphere coupling downstream of soil moisture conditions. Overall, soil moisture increases the variability of the convective margin, although how it does so is nontrivial. In particular, there is an asymmetry in displacements of the convective margin between anomalous inflow and outflow conditions that is absent when soil moisture is not included. Furthermore, the simple cases presented here illustrate how margin sensitivity depends strongly on the interplay of factors, including net top-of-the-atmosphere radiative heating, the statistics of inflow wind, and the convective parameterization.


2017 ◽  
Vol 50 ◽  
pp. 293-307 ◽  
Author(s):  
Naoki Hanawa ◽  
Masanori Kuniyoshi ◽  
Masaaki Miyatake ◽  
Shigeka Yoshimoto

2009 ◽  
Vol 23 (1) ◽  
pp. 71 ◽  
Author(s):  
Wahyuni Apri Astuti ◽  
Muhammad Musiyam

This research is based on the facts: first that, Boyolali is one of the regions which implement intensively many kinds of program in solving the poverty which gets the finance from APBD, central government and international institutions, eventhough the proportion of the poor society increases significantly.The proportion of poor society increases 20,8% in 2002 becomes 38,26% in 2006. Second, seen from the regional development indicator, it is shown that between one region and the others has various levels of the varieties of development.The objectives of this research are: first, the understanding of the distribution and of the poverty level in this region. Second, the understanding of the relationship between distribution of poverty level and the regional development level. Third, the understanding of the factors which influence the regional development. The method used in this research is secondary data analysis. The analysis unit of this research is village. The data resources are taken from the report of the identification result of poor families and the primary data is taken from BAPPEDA Boyolali. The primary data is a number of poor families, the regional scope and the use of farmland, the long street to account the regional accessibilities and the number and the distribution of social and economical facility in each village. The result is presented on the map with the analysis unit of the village. The represented map are the distribution level of poverty per village. To determine the relationship between the level of poverty and regional development uses the technique of qualitative and quantitative analysis. The qualitative analysis technique used is the analysis of the map of poverty distribution, analysis map of regional development and harmonious relationship between the level of regional development and poverty. The quantitative analysis technique used is the analysis of correlation statistic product moment.The results of this research are: first, there is distribution variation of poverty level, there is relationship between distribution of poverty level and natural resources endowment.The region with lower resources endowment (up land region) have higher poverty level than the region with higher natural resources endowment (law land region) and conversel. Second, there is negative relationship between regional development level and poverty level.Third, the factors which influence the level of regional development are the economical and social facility of the region and accessibilities.


1980 ◽  
Vol 100 ◽  
pp. 11-15
Author(s):  
N Henriksen

The second season of a three year systematic field mapping programme in the Peary Land region, north of latitude 81°N and east of longitude 40° W, was carried out from June to August 1979. The aim of the programme is to produce a 1:500000 map sheet of eastern North Greenland and to investigate the geological framework of the region. As in 1978 the expedition was carried out in cooperation with a surveying group from the Geodetic Institute, Copenhagen, who mainly worked in the region west of Peary Land establishing ground control points for a new topographic map of North Greenland.


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