MONITORING SUMMER SOLAR ULTRAVIOLET (UV) RADIATION ON THE GROUND LEVEL OVER ARDABIL-SAREIN, NW IRAN

نویسندگان

چکیده

Abstract. The UV radiation level at the Earth’s surface is generally affected by several factors such as time, geographic location, and climate. first observations of solar ever made in NW Iran, obtained June 2019 are reported this work. analysis hourly values irradiances measured study area reveals significant diurnal variation during daylight hours, with lower morning afternoon higher around noon. Mean (A+B) ranged from 2755 to 10434 µW/cm2 an average value being about 7960 µW/cm2. (C) 40 91 76 results a short but intense measurement campaign Ardabil-Sarein indicate trends for geographical latitude, longitude, altitude measurements. intensity associated longitude (r2= 0.15 (A+B); r2= 0.13 (C)). Furthermore, varies local latitude area. There strong linear relationship between trend rising increasing obtained. A decrease zenith (°) was observed. However, correlation azimuth not significant. Understanding influencing near-surface through systematic ground-based will help determine whether long-term changes occur result cloud cover or climate change, how specific it means identifying causes.

برای دانلود باید عضویت طلایی داشته باشید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Solar ultraviolet radiation on the ground level of Isfahan

Introduction: Ultraviolet (UV) radiation affects human organs such as skin, eyes and immune system, as well as animals and plants. The main natural source of UV radiation is the Sun. To study the effects of solar UV radiation there is a need to quantify variations of solar energy received on the earth surface at different intervals. Materials and Methods: To measure UV radiation a broadband fib...

متن کامل

solar ultraviolet radiation on the ground level of isfahan

introduction: ultraviolet (uv) radiation affects human organs such as skin, eyes and immune system, as well as animals and plants. the main natural source of uv radiation is the sun. to study the effects of solar uv radiation there is a need to quantify variations of solar energy received on the earth surface at different intervals. materials and methods: to measure uv radiation a broadband fib...

متن کامل

Solar ultraviolet-B radiation monitoring in Khorram Abad city in Iran

Background: The increasing evidences show that global depletion of stratospheric ozone layer is caused by pollutant and growing incidence of the skin cancer and cataract is related to the amounts of solar UV radiation reaching the earth ׳s surface. Therefore, the main driving force behind such efforts has been the lack of an appropriate network in scope monitoring of the terrestrial UV...

متن کامل

Solar ultraviolet exposures at ground level in tree shade during summer in south east Queensland.

Data are presented on the effect of the tree canopy transmittance in the visible waveband (VT), canopy width, height and height of the start of the tree canopy (CH) on the solar UV in tree shade on a horizontal plane at ground level during a Southern Hemisphere summer. Of these factors, the VT and CH have an influence on the UV irradiances in the tree shade. The shade ratios (UV in tree shade t...

متن کامل

Measurement of solar ultraviolet radiation in Yazd, Iran

Background: Ultraviolet (UV) radiation is divided into three regions: UVA, UVB, and UVC. Both the quality and quantity of solar UV radiation vary with various factors including the elevation of the sun above the horizon, as well as absorption and scattering of UV photons by molecules in the atmosphere, notably ozone and clouds. It is clear that whereas a moderate amount of UV exposure ...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

ژورنال

عنوان ژورنال: ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences

سال: 2023

ISSN: ['2194-9042', '2194-9050', '2196-6346']

DOI: https://doi.org/10.5194/isprs-annals-x-4-w1-2022-327-2023