Severity: Warning
Message: file_get_contents(https://...@gmail.com&api_key=61f08fa0b96a73de8c900d749fcb997acc09&a=1): Failed to open stream: HTTP request failed! HTTP/1.1 429 Too Many Requests
Filename: helpers/my_audit_helper.php
Line Number: 176
Backtrace:
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 176
Function: file_get_contents
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 250
Function: simplexml_load_file_from_url
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 3122
Function: getPubMedXML
File: /var/www/html/application/controllers/Detail.php
Line: 575
Function: pubMedSearch_Global
File: /var/www/html/application/controllers/Detail.php
Line: 489
Function: pubMedGetRelatedKeyword
File: /var/www/html/index.php
Line: 316
Function: require_once
Dry deposition of ozone (O) to vegetation is an important pathway for its removal from the troposphere, and it can lead to adverse effects in plants and changes in climate. However, our mechanistic understanding of O dry deposition is insufficient to adequately account for it in global and regional models, primarily because this process is highly complicated by feedback mechanisms and sensitivity to specific characteristics of vegetative environment and atmospheric dynamics and composition. We hypothesized that measuring dry deposition of O to vegetation near the Eastern Mediterranean (EM) coast, where large variations in meteorological conditions and photochemical air pollution frequently occur, would enable identifying the mechanisms controlling O deposition to vegetation. Moreover, we have only limited knowledge of O deposition to vegetation occurring near a coastline, under air pollution, or in the EM. This study investigated O deposition to mixed Mediterranean vegetation between the summers of 2015 and 2017, 3.6 km away from the EM coast, using the eddy covariance technique to quantify vertical flux of O and its partitioning to stomatal and non-stomatal flux, concurrent with nitrogen oxide (NO), sulfur dioxide and carbon monoxide. Surprisingly, nighttime O-deposition velocity (V) was smaller than daytime V by only ~20-37% on average for all measurement periods, primarily related to moderate nighttime atmospheric stability due to proximity to the seashore. We provide evidence for the role of sea-salt aerosols in enhancing O deposition via surface-wetness buildup at low relative humidity near the coast, and for daytime enhancement of O deposition by the combined effects of biogenic volatile organic compound emission and surface-wetness buildup. We further show that NO emitted from elevated emission sources can reduce O deposition, and even lead to a positive O flux, demonstrating the importance of adequately taking into account the impact of air pollution on O deposition to vegetation.
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http://dx.doi.org/10.1016/j.scitotenv.2018.07.037 | DOI Listing |
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