Asia precipitation tripole during boreal summer: Anomalous water vapour transport along the “Southern Silk Road”

2020 ◽  
Author(s):  
Mengke Zhang ◽  
Dachao Jin ◽  
Xi Liu ◽  
Xudong Wang ◽  
Yang Xia
Keyword(s):  
Water Vapour ◽  
Silk Road ◽  
Boreal Summer ◽  
Vapour Transport ◽  
Water Vapour Transport ◽  
Anomalous Water

scholarly journals Water vapour transport in the tropical tropopause region in coupled Chemistry-Climate Models and ERA-40 reanalysis data

2009 ◽  
Vol 9 (8) ◽  
pp. 2679-2694 ◽  
Author(s):  
Stefanie Kremser ◽  
Ingo Wohltmann ◽  
Markus Rex ◽  
Ulrike Langematz ◽  
Martin Dameris ◽  
...  
Keyword(s):  
Water Vapour ◽  
Geographical Distribution ◽  
Indian Monsoon ◽  
Reanalysis Data ◽  
Boreal Summer ◽  
Residence Times ◽  
Vapour Transport ◽  
Water Vapour Transport ◽  
Tropical Tropopause ◽  
La Nina

Abstract. In this study backward trajectories from the tropical lower stratosphere were calculated for the Northern Hemisphere (NH) winters 1995–1996, 1997–1998 (El Niño) and 1998–1999 (La Niña) and summers 1996, 1997 and 1999 using both ERA-40 reanalysis data of the European Centre for Medium-Range Weather Forecast (ECMWF) and coupled Chemistry-Climate Model (CCM) data. The calculated trajectories were analysed to determine the distribution of points where individual air masses encounter the minimum temperature and thus minimum water vapour mixing ratio during their ascent through the tropical tropopause layer (TTL) into the stratosphere. The geographical distribution of these dehydration points and the local conditions there determine the overall water vapour entry into the stratosphere. Results of two CCMs are presented: the ECHAM4.L39(DLR)/CHEM (hereafter: E39/C) from the German Aerospace Center (DLR) and the Freie Universität Berlin Climate Middle Atmosphere Model with interactive chemistry (hereafter: FUB-CMAM-CHEM). In the FUB-CMAM-CHEM model the minimum temperatures are overestimated by about 9 K in NH winter and about 3 K in NH summer, resulting in too high water vapour entry values compared to ERA-40. However, the geographical distribution of dehydration points is fairly similar to ERA-40 for NH winter 1995–1996 and 1998–1999. The distribution of dehydration points in the boreal summer 1996 suggests an influence of the Indian monsoon upon the water vapour transport. The E39/C model displays a temperature bias of about +5 K. Hence, the minimum water vapour mixing ratios are higher relative to ERA-40. The geographical distribution of dehydration points is fairly well in NH winter 1995–1996 and 1997–1998 with respect to ERA-40. The distribution is not reproduced for the NH winter 1998–1999 (La Niña event) compared to ERA-40. There is an excessive water vapour flux through warm regions e.g. Africa in the NH winter and summer. The possible influence of the Indian monsoon on the transport is not seen in the boreal summer 1996. Further, the residence times of air parcels in the TTL were derived from the trajectory calculations. The analysis of the residence times reveals that in both CCMs residence times in the TTL are lower compared to ERA-40 and the seasonal variation is hardly present.

Gas and water vapour transport through polymer based protective materials for stone monuments: Fluorinated polyurethanes

1998 ◽  
Vol 31 (2) ◽  
pp. 104-110 ◽  
Author(s):  
V. Antonucci ◽  
C. Mastrangeli ◽  
G. Mensitieri ◽  
M. A. Del Nobile ◽  
L. Nicolais
Keyword(s):  
Water Vapour ◽  
Vapour Transport ◽  
Stone Monuments ◽  
Water Vapour Transport

Water vapour transport in a soil column in the presence of an osmotic gradient

Geoderma ◽  
2018 ◽  
Vol 315 ◽  
pp. 199-207 ◽  
Author(s):  
Seyed Mohamad Mahdavi ◽  
Mohammad Reza Neyshabouri ◽  
Haruyuki Fujimaki
Keyword(s):  
Water Vapour ◽  
Soil Column ◽  
Osmotic Gradient ◽  
Vapour Transport ◽  
Water Vapour Transport

Precipitation in the Madeira Island over a 10-year period and the meridional water vapour transport during the winter seasons

2015 ◽  
Vol 35 (13) ◽  
pp. 3748-3759 ◽  
Author(s):  
Flavio Tiago Couto ◽  
Rui Salgado ◽  
Maria João Costa ◽  
Victor Prior
Keyword(s):  
Water Vapour ◽  
Vapour Transport ◽  
Madeira Island ◽  
Water Vapour Transport
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