干旱区生态环境知识资源中心

RATIONALE Isotope (d18O and d2H values) ratios in precipitation have been central to understanding changes in Earth’s climate as recorded in ice, coral, speleothems, lake varves and long-lived plants. Understanding how climate phases (i.e. ENSO) affect the spatial and temporal patterns of d18O and d2H values in precipitation has, however, been uncertain across the USA. METHODS A spatial precipitation isotope network (USNIP) has been established that aims to: (1) characterize the d18O, d2H and d-excess values in precipitation across the USA with the highest spatially dense network of measurements yet undertaken; (2) quantify the annual and seasonal patterns of precipitation d18O and d2H values that may be affected by ENSO climate phases; and (3) provide a new isotope database for scientific studies that can be incorporated into NEON, BASIN, GNIP, and IsoMAP. RESULTS On average, precipitation d18O and d2H values are very low in the northern Rocky Mountain region (similar to -15 parts per thousand d18O, and?similar to?-120 parts per thousand d2H), and precipitation d18O and d2H values are relatively higher along the Gulf Coast (similar to -5 parts per thousand d18O and -10 parts per thousand d2H) and in the Southeast. During El Nino periods the precipitation d18O and d2H values are lowest in northwest Montana, with precipitation that is depleted in 18O and 2H extending into northern Colorado, while moisture that is enriched in 18O and 2H continues to dominate the Gulf Coast. The annual average differences between the climate phases generally show especially depleted 18O and 2H in precipitation across the Rocky Mountain region during El Nino, compared with Neutral periods. CONCLUSIONS Detailed spatial and seasonal patterns of d18O, d2H and d-excess values provide fine-scale resolution not previously recognized. Climate phases of ENSO have major effects on the spatial patterns of d18O, d2H and d-excess values, being especially important on a seasonal basis in the Desert Southwest. Copyright (C) 2012 John Wiley & Sons, Ltd.