LCZO -- Stable Isotopes -- Stable Isotope (δ18O and δ2H) Data -- Puerto Rico -- (1994-2013)


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Owners: CZO LuquilloCZO National
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Created: Nov 19, 2019 at 4:50 a.m.
Last updated: Apr 23, 2020 at 2:16 p.m.
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Abstract

Like many mountainous areas in the tropics, watersheds in the Luquillo Mountains of eastern Puerto Rico have abundant rainfall and stream discharge and provide much of the water supply for the densely populated metropolitan areas nearby. Projected changes in regional temperature and atmospheric dynamics as a result of global warming suggest that water availability will be affected by changes in rainfall patterns. It is essential to understand the relative importance of different weather systems to water supply to determine how changes in rainfall patterns, interacting with geology and vegetation, will affect the water balance. To help determine the links between climate and water availability, stable isotope signatures of precipitation from different weather systems were established to identify those that are most important in maintaining streamflow and groundwater recharge. Precipitation stable isotope values in the Luquillo Mountains had a large range, from fog/cloud water with δ2H, δ18O values as high as +12 ‰, −0.73 ‰ to tropical storm rain with values as low as −127 ‰, −16.8 ‰. Temporal isotope values exhibit a reverse seasonality from those observed in higher latitude continental watersheds, with higher isotopic values in the winter and lower values in the summer. Despite the higher volume of convective and low-pressure system rainfall, stable isotope analyses indicated that under the current rainfall regime, frequent trade -wind orographic showers contribute much of the groundwater recharge and stream base flow. Analysis of rain events using 20 years of 15 -minute resolution data at a mountain station (643 m) showed an increasing trend in rainfall amount, in agreement with increased precipitable water in the atmosphere, but differing from climate model projections of drying in the region. The mean intensity of rain events also showed an increasing trend. The determination of recharge sources from stable isotope tracers indicates that water supply will be affected if regional atmospheric dynamics change trade- wind orographic rainfall patterns in the Caribbean.

For more data a USGS open file report is available: Stable Isotope (δ18O and δ2H) Data for Precipitation, Stream Water, and Groundwater in Puerto Rico http://dx.doi.org/10.3133/ofr20141101

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Northeastern Puerto Rico and the Luquillo Mountains, Rio Icacos, East Peak, Rio Mameyes, Puerto Rico
North Latitude
18.4119°
East Longitude
-65.6751°
South Latitude
18.1707°
West Longitude
-65.8473°

Temporal

Start Date: 08/31/1994
End Date: 03/26/2013
Leaflet Map data © OpenStreetMap contributors

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How to Cite

Scholl, M. A., A. Torres-Sanchez, M. Rosario-Torres (2020). LCZO -- Stable Isotopes -- Stable Isotope (δ18O and δ2H) Data -- Puerto Rico -- (1994-2013), HydroShare, http://www.hydroshare.org/resource/3b0ff71572634812b20ca9ee992cf44c

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

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