Pii: S0022-1694(00)00144-x
نویسنده
چکیده
This paper presents three multivariate geostatistical algorithms for incorporating a digital elevation model into the spatial prediction of rainfall: simple kriging with varying local means; kriging with an external drift; and colocated cokriging. The techniques are illustrated using annual and monthly rainfall observations measured at 36 climatic stations in a 5000 km region of Portugal. Cross validation is used to compare the prediction performances of the three geostatistical interpolation algorithms with the straightforward linear regression of rainfall against elevation and three univariate techniques: the Thiessen polygon; inverse square distance; and ordinary kriging. Larger prediction errors are obtained for the two algorithms (inverse square distance, Thiessen polygon) that ignore both the elevation and rainfall records at surrounding stations. The three multivariate geostatistical algorithms outperform other interpolators, in particular the linear regression, which stresses the importance of accounting for spatially dependent rainfall observations in addition to the colocated elevation. Last, ordinary kriging yields more accurate predictions than linear regression when the correlation between rainfall and elevation is moderate (less than 0.75 in the case study). q 2000 Elsevier Science B.V. All rights reserved.
منابع مشابه
Pii: S0022-1694(00)00303-6
Isotopic tracer and temperature measurements at large volume cold springs in the central Oregon Cascades are used to understand the pattern of groundwater flow. Standard oxygen and hydrogen isotope interpretations are used to determine the mean recharge elevation for springs. Carbon and helium isotopes are used to measure the component of dissolved magmatic gas in the spring waters. Inferences ...
متن کاملPii: S0022-4073(98)00144-7
A recently developed version of the discrete-ordinates method is used along with elementary numerical linear-algebra techniques to establish an e$cient and especially accurate solution to what can be called Chandrasekhar's basic problem in radiative transfer, namely the problem of computing the radiation intensity in a "nite plane-parallel layer illuminated by an incident beam of radiation and ...
متن کاملPii: S0022-1694(00)00336-x
Trends in ̄ood and low ̄ows in the US were evaluated using a regional average Kendall's S trend test at two spatial scales and over two timeframes. Field signi®cance was assessed using a bootstrap methodology to account for the observed regional cross-correlation of stream ̄ows. Using a 5% signi®cance level, we found no evidence of trends in ̄ood ̄ows but did ®nd evidence of upward trends in low...
متن کاملPii: S0022-1694(00)00198-0
The initial soil water content affects wetting front instability. A series of experiments were conducted where water was infiltrated into a 20/30 sand with initial volumetric water contents of 0, 0.005, 0.01, 0.015, 0.02, 0.03, 0.04 and 0.047 cm/cm. Both water content and matric potential were measured. Water content was measured with Synchrotron X-rays at the Cornell High Energy Synchrotron So...
متن کاملPii: S0022-3697(98)00144-9
In this paper, we review some of the work our group has done in the past few years to obtain the electron self-energy of high temperature superconductors by analysis of angle-resolved photoemission data. We focus on three examples which have revealed: (1) a d-wave superconducting gap, (2) a collective mode in the superconducting state, and (3) pairing correlations in the pseudogap phase. In eac...
متن کامل