Ahmed saber taha mitwali soliman
Lecturer
Analysis of spatial and temporal variation of precipitable water vapor using COSMIC radio occultation observations over Egypt
• 2022
Publication Information
Authors
Abd Elrahman Yassien; Ashraf El-Kutb Mousa; Mostafa Rabah;Ahmed Saber
a,
⇑, Mohamed Zhran
Keywords
COSMIC data
Precipitable water vapor
GNSS
Radio occultation
Radiosonde
Journal
Not Available
Publisher
Not Available
Volume
Not Available
Issue
Not Available
Pages
Not Available
publication.type
Local
Paper Link
Not Available
Supplementary Materials
Not Available
Abstract
Precipitable water vapor (PWV) is a meteorological variable that impacts the major atmospheric processes.
It is a non-homogeneous variable that differs spatially and temporally. The spatial and temporal
variability of the PWV in Egypt is investigated in this study using Global Navigation Satellite Systems
(GNSS) Radio Occultation (RO) from 2006 to 2021. The GNSS RO technique was used to obtain PWV values;
the validation results agree with the radiosonde technique. From the statistical results, the mean
bias is 0.1846 mm. The PWV has a latitudinal style in which it is inversely proportional to latitude. So,
it is evident that higher PWV occurs at low latitudes. However, some PWV values are higher over sites
near the coast of the Mediterranean Sea. No clear and direct relationship is found between PWV and longitude.
So, PWV is mainly dependent on latitude. The annual mean PWV values over Egypt range from
9.23 mm to 13.51 mm. The higher values of PWV are in the summer season between 10.74 mm and
21.55 mm. While the PWV values are in the winter season range from 6.84 mm to 9.94 mm. The highest
values of PWV occur in August between 12.35 mm and 23.35 mm and the lowest values of PWV are in
January and February ranging from 5.62 mm to 11.05 mm. PWV values are higher during the day and
lower at night.
It is a non-homogeneous variable that differs spatially and temporally. The spatial and temporal
variability of the PWV in Egypt is investigated in this study using Global Navigation Satellite Systems
(GNSS) Radio Occultation (RO) from 2006 to 2021. The GNSS RO technique was used to obtain PWV values;
the validation results agree with the radiosonde technique. From the statistical results, the mean
bias is 0.1846 mm. The PWV has a latitudinal style in which it is inversely proportional to latitude. So,
it is evident that higher PWV occurs at low latitudes. However, some PWV values are higher over sites
near the coast of the Mediterranean Sea. No clear and direct relationship is found between PWV and longitude.
So, PWV is mainly dependent on latitude. The annual mean PWV values over Egypt range from
9.23 mm to 13.51 mm. The higher values of PWV are in the summer season between 10.74 mm and
21.55 mm. While the PWV values are in the winter season range from 6.84 mm to 9.94 mm. The highest
values of PWV occur in August between 12.35 mm and 23.35 mm and the lowest values of PWV are in
January and February ranging from 5.62 mm to 11.05 mm. PWV values are higher during the day and
lower at night.
