scholarly journals Continuous Measurement of the Salinity of Sea Water by means of High Frequency Apparatus

1956 ◽  
Vol 77 (1) ◽  
pp. 140-144
Author(s):  
Sôichirô Musha ◽  
Makoto Munemori ◽  
Mitsuo Itô ◽  
Masami Takeda ◽  
Shôichirô Nakamura ◽  
...  
The Lancet ◽  
1912 ◽  
Vol 180 (4659) ◽  
pp. 1677-1678
Author(s):  
S.C. Damoglou

1963 ◽  
Vol 5 (6) ◽  
pp. 361-362
Author(s):  
S. F. Solodovnik

2021 ◽  
Vol 4 (3) ◽  

In Nature, 570, 200 (2019), Minev and co-authors’ experiment shows how to deterministically “catch and reverse a quantum jump mid-flight” in a continuously-observed Rabi-stimulated qubit. Its interpretation is in debate (La Recherche, 555, 40, (2020)). We show that the quantum Zeno effect (QZE) of continuous measurement —by use of photon emission from a 3rd high-rate monitored ancilla level— can be described by an action-angle canonical transformation of the original Hamiltonian dynamical system (HDS) theory of QZE. Then energy whose mean value yields the well-known resonant Rabi harmonic dynamics is actually defined by large-amplitude high-frequency oscillations of the internal as well as of the overall phase of the two-level system. By making use of their standard deviation, we show that the separatrix crossing of the HDS trajectory yields the quantized action nh where n = 1, 2, 3 .... Therefore, the jump dynamics observed in Minev et al. experiment belongs to a series of discrete quantum jumps: it corresponds in this experiment to n = 3.


2007 ◽  
Vol 54 (1) ◽  
pp. 75-84 ◽  
Author(s):  
Koutaro Tsubaki ◽  
Shigenao Maruyama ◽  
Atsuki Komiya ◽  
Hiroaki Mitsugashira

2018 ◽  
Vol 48 (3) ◽  
pp. 723-738 ◽  
Author(s):  
Kai Håkon Christensen ◽  
Ann Kristin Sperrevik ◽  
Göran Broström

AbstractA high-resolution reanalysis of the circulation in the Kattegat and Skagerrak is used to investigate the mechanisms that control the variability in the onset of the Norwegian Coastal Current. In the reanalysis, the authors have used all available in situ and remote sensing observations of salinity and temperature and use surface current observations from two coastal high-frequency radars that were ideally placed to monitor the exchange between the two basins. This study finds a strong correlation between the variability in the wind forcing in the Skagerrak and the transport in the Norwegian Coastal Current through the Torungen–Hirtshals section. Two cases with winds into and out of the Skagerrak are studied in more detail, and the results suggest asymmetries in the forcing mechanisms. For winds out of the Skagerrak, strong outflows of Baltic Sea Water associated with a deflection of the Kattegat–Skagerrak Front may disrupt local processes in the Skagerrak, which is not accounted for in previously published conceptual models for the variability of the coastal currents in this region.


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