z-logo
Premium
A large terrestrial source of methyl iodide
Author(s) -
Sive Barkley C.,
Varner Ruth K.,
Mao Huiting,
Blake Donald R.,
Wingenter Oliver W.,
Talbot Robert
Publication year - 2007
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2007gl030528
Subject(s) - middle latitudes , biome , methyl iodide , environmental science , atmosphere (unit) , atmospheric sciences , flux (metallurgy) , vegetation (pathology) , mixing ratio , climatology , geology , meteorology , geography , ecosystem , ecology , chemistry , medicine , organic chemistry , pathology , medicinal chemistry , biology
We have identified terrestrial sources of methyl iodide (CH 3 I) and assessed their importance in its atmospheric budget using a synthesis of field observations. Measurements include those from NASA DC‐8 research flights over the United States and the North Atlantic, the AIRMAP long‐term ground‐observing network in New England, and a field campaign at Duke Forest, North Carolina. We found an average CH 3 I flux of ∼2,700 ng m −2 d −1 to the atmosphere from midlatitude vegetation and soils, a value similar in magnitude to previous estimates of the oceanic source strength. The large‐scale aircraft measurements of vertical profiles over the continental U.S. showed CH 3 I‐mixing ratios comparable to and greater than those observed over the North Atlantic. Overall, midlatitude terrestrial biomes appear to contribute 33 Gg yr −1 to the CH 3 I global budget.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom