2020
DOI: 10.1080/10256016.2020.1815722
|View full text |Cite
|
Sign up to set email alerts
|

Atmospheric constraints on δ18O and d-excess in precipitation at the middle latitude in the southwestern Atlantic region

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2020
2020
2022
2022

Publication Types

Select...
3

Relationship

1
2

Authors

Journals

citations
Cited by 3 publications
(1 citation statement)
references
References 26 publications
0
1
0
Order By: Relevance
“…Light isotopes are depleted in advance while heavy isotopes in raindrops are enriched [4][5][6], showing that there has been a decrease in the deuterium excess or d which equals δ 2 H − 8 × δ 18 O [7]. The evaporation and condensation are impacted by the different climate parameters [8,9], and the deuterium excess in meteoric water is also sensitive to these climate conditions [10][11][12], causing that the deuterium excess can be a useful indicator to trace the source of water vapor and assess the potential existence of the sub-cloud evaporation [13][14][15][16].…”
Section: Introductionmentioning
confidence: 99%
“…Light isotopes are depleted in advance while heavy isotopes in raindrops are enriched [4][5][6], showing that there has been a decrease in the deuterium excess or d which equals δ 2 H − 8 × δ 18 O [7]. The evaporation and condensation are impacted by the different climate parameters [8,9], and the deuterium excess in meteoric water is also sensitive to these climate conditions [10][11][12], causing that the deuterium excess can be a useful indicator to trace the source of water vapor and assess the potential existence of the sub-cloud evaporation [13][14][15][16].…”
Section: Introductionmentioning
confidence: 99%