Anti-contiguity Crosslinguistically

2020 ◽  
pp. 100-122
Author(s):  
Jason Kandybowicz

This chapter concludes the book by considering Anti-contiguity in a cross-linguistic context. It is shown that the proposal can be successfully applied to derive asymmetries in wh- in-situ distribution beyond the West African languages considered in Chapters 2–4. The chapter focuses on thirteen languages from diverse language families (Romance, Bantu, and Indo-Aryan, among others) and considers the implications of data from these languages for the final formulation of the Anti-contiguity condition. On the basis of these considerations, the Anti-contiguity constraint is parameterized. Among the languages considered against the backdrop of the Anti-contiguity proposal in this chapter are French; Spanish; Catalan; Zulu; Bàsàá; Duala; Shona; Lubukusu; Kiitharaka; Hindi-Urdu; Bangla; Iraqi Arabic; and Malayalam.

Author(s):  
Alain Kihm

Substratal influences as an explanation for creolization (and language change generally) often fail to convince for one major reason, namely that, in most cases, the possible substratum for a given creole language is now separated from the site where creolization took place by a wide historical and geographical gap. This, for example, is the case of the West African languages vis-à-vis the Caribbean Creoles.


1963 ◽  
Vol 6 (03) ◽  
pp. 30-31
Author(s):  
Joseph Greenberg

The Third West African Languages Congress took place in Freetown, Sierra Leone, from March 26 to April 1, 1963. This was the third of the annual meetings of those interested in West African languages sponsored by the West African Languages Survey, previous meetings having been held in Accra (1961) and Dakar (1962). The West African Languages Survey is a Ford Foundation project. Additional financial assistance from UNESCO and other sources contributed materially to the scope and success of the meeting. This meeting was larger than previous ones both in attendance and in number of papers presented and, it may be said, in regard to the scientific level of the papers presented. The official participants, seventy-two in number, came from virtually every country in West Africa, from Western European countries and from the United States. The linguistic theme of the meeting was the syntax of West African languages, and a substantial portion of the papers presented were on this topic. In addition, there was for the first time at these meetings a symposium on the teaching of English, French and African languages in Africa. The papers of this symposium will be published in the forthcoming series of monographs planned as a supplement to the new Journal of West African Languages. The other papers are to appear in the Journal of African Languages edited by Jack Berry of the School of Oriental and African Studies.


2021 ◽  
Author(s):  
Ivan Tadic ◽  
Clara Nussbaumer ◽  
Birger Bohn ◽  
Hartwig Harder ◽  
Daniel Marno ◽  
...  

Abstract. Mechanisms of tropospheric ozone (O3) formation are generally well understood. However, studies reporting on net ozone production rates (NOPRs) directly derived from in-situ observations are challenging, and are sparse in number. To analyze the role of nitric oxide (NO) in net ozone production in the upper tropical troposphere above the Atlantic Ocean and the West African continent, we present in situ trace gas observations obtained during the CAFE-Africa (Chemistry of the Atmosphere: Field Experiment in Africa) campaign in August and September 2018. The vertical profile of in situ measured NO along the flight tracks reveals lowest NO mixing ratios of less than 20 pptv between 2 and 8 km altitude and highest mixing ratios of 0.15–0.2 ppbv above 12 km altitude. Spatial distribution of tropospheric NO above 12 km altitude shows that the sporadically enhanced local mixing ratios (> 0.4 ppbv) occur over the West African continent, which we attribute to episodic lightning events. Measured O3 shows little variability in mixing ratios at 60–70 ppbv, with slightly decreasing and increasing tendencies towards the boundary layer and stratosphere, respectively. Concurrent measurements of CO, CH4, OH and HO2 and H2O enable calculations of NOPRs along the flight tracks and reveal net ozone destruction at −0.6 to −0.2 ppbv h−1 below 6 km altitude and balance of production and destruction around 7–8 km altitude. We report vertical average NOPRs of 0.2–0.4 ppbv h−1 above 12 km altitude with NOPRs occasionally larger than 0.5 ppbv h−1 over West Africa coincident with enhanced NO. We compare the observational results to simulated data retrieved from the general circulation ECHAM/MESSy Atmospheric Chemistry (EMAC) model. Although the comparison of mean vertical profiles of NO and O3 indicates good agreement, local deviations between measured and modelled NO are substantial. The vertical tendencies in NOPRs calculated from simulated data largely reproduce those from in situ experimental data. However, the simulation results do not agree well with NOPRs over the West African continent. Both measurements and simulations indicate that ozone formation in the upper tropical troposphere is NOx-limited.


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