scholarly journals Correlation with spontaneous pneumothorax and weather change, especially warm front approaching

2021 ◽  
Vol 13 (3) ◽  
pp. 1584-1591
Author(s):  
Yuka Kaneko ◽  
Yoshihiro Utsushikawa ◽  
Hiroyuki Deguchi ◽  
Makoto Tomoyasu ◽  
Satoshi Kudo ◽  
...  
1991 ◽  
Vol 27 (3) ◽  
pp. 363
Author(s):  
Dong Wook Sung ◽  
Seung Hyae Jung ◽  
Yup Yoon ◽  
Jae Hoon Lim ◽  
Kyu Soek Cho ◽  
...  

1934 ◽  
Vol 2 (1) ◽  
pp. 44
Author(s):  
S. H. Martin ◽  
C.M. Pak ◽  
S. H. Pak

2000 ◽  
Vol 51 (6) ◽  
pp. 420-425 ◽  
Author(s):  
Ichirou Motomura ◽  
Hiroki Fujihara ◽  
Yoshio Hamashima ◽  
Kaori Hashimoto ◽  
Takemasa Kanazawa ◽  
...  

2018 ◽  
Vol 69 (9) ◽  
pp. 2591-2593
Author(s):  
Cristina Grigorescu ◽  
Liviu Ciprian Gavril ◽  
Laura Gavril ◽  
Tiberiu Lunguleac ◽  
Bogdan Mihnea Ciuntu ◽  
...  

Diagnosis of primary or idiopathic spontaneous pneumothorax is one of exclusion, and in fact defines an entity that may have a difficult or impossible cause to be highlighted by current means, we consider it appropriate to study these etiopathogenic aspects. There is a definite association between alpha-1 antitrypsin deficiency and pulmonary emphysema and indirect spontaneous pneumothorax secondary to an emphysematous pulmonary lesion. Dose of alpha-1 antitrypsin is an immunoturbinimetric method for in vitro determination of alpha-1 antitrypsin in human serum and plasma. This product is calibrated to be used for the Daytona RX analyzer. The serum level of alpha-1-antitrypsin is not a determining factor in the postoperative evolution characterized by the interval until air loss disappears, but certainly exerts some influence, the exact level of which remains to be determined.


1988 ◽  
Vol 19 (1) ◽  
pp. 53-64 ◽  
Author(s):  
C. Corradini ◽  
F. Melone

Evidence is given of the distribution of pre-warm front rainfall at the meso-γ scale, together with a discussion of the main mechanisms producing this variability. An inland region in the Mediterranean area is considered. The selected rainfall type is commonly considered the most regular inasmuch as it is usually unaffected by extended convective motions. Despite this, within a storm a large variability in space was observed. For 90% of measurements, the typical deviations from the area-average total depth ranged from - 40 to 60 % and the storm ensemble-average rainfall rate over an hilly zone was 60 % greater than that in a contiguous low-land zone generally placed upwind. This variability is largely explained in terms of forced uplift of air mass over an envelope type orography. For a few storms smaller orographic effects were found in locations influenced by an orography with higher slopes and elevations. This feature is ascribed to the compact structure of these mountains which probably determines a deflection of air mass in the boundary layer. The importance of this type of analysis in the hydrological practice is also emphasized.


1950 ◽  
Vol 19 (2) ◽  
pp. 167-198 ◽  
Author(s):  
Lyman A. Brewer ◽  
Frank S. Dolley ◽  
Byron H. Evans

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