1                  Buckler-White, et al., Proc Natl Acad Sci U S A 98:658-663, 2001, J.

2 ):69-88 and Saranathan V, et al. (2010) Proc Natl Acad Sci USA 107(26):11676-11681, where the two ena

3                                         Proc Natl Acad Sci USA 112, 15838-15843] no longer found an a

4                                         Proc Natl Acad Sci USA 112, 15838-15843], who suggested that

5  PNAS [Cote S, House J, Willer R (2015) Proc Natl Acad Sci USA 112:15838-15843] showed that higher in

6 nd Levitt [Ufimtsev IS, Levitt M (2019) Proc Natl Acad Sci USA, 10.1073/pnas.1821512116], we presente

7 04, 18866-18870; Raupach et al. [2007], Proc Natl Acad Sci USA, 104, 10288-10293).

8 lly since 2007 (Canadell et al. [2007], Proc Natl Acad Sci USA, 104, 18866-18870; Raupach et al. [200

9  moisture sources: the North Atlantic Ocean (NATL) and Mediterranean Sea (MED).

10 ting oligonucleotides, these components form NaTl-type colloidal crystalline structures containing in

11 ally coming at high pressure to a diamondoid NaTl-type LiB.

12 stern Europe, while that associated with the NATL will decrease over western Europe and Africa.

13 By the end of the century, moisture from the NATL will increase precipitation over eastern North Amer