Jeo-İstatistik'te Kullanılan Temel Kriging Yöntemleri

Year 2017, Volume: 27 Issue: 1, 10 - 20, 31.03.2017

Pınar Bostan

https://doi.org/10.29133/yyutbd.305093

Cited By: 3

Abstract

Çevresel, hidrolojik, tarımsal
ve benzer çalışmalara ait ölçümler dünya üzerinde yapılmış noktasal gözlemlere
dayanır. Yağış ve sıcaklık değerleri meteorolojik istasyonlarda, toprak
karakteristiği toprak örneklerinden ve göl kirliliği gölden alınan örneklerden
ölçülür. Bunlar noktasal olarak yapılan mekânsal ölçümlere örnektir. Belli
noktalardan örnekler alarak veya belirgin yerlerden ölçüm yaparak sınırlı
sayıda ölçüm yapabiliriz. Ancak ilgilendiğimiz değişkenin dünyanın her
noktasında ya da belli büyüklükteki bir alan üzerinde ölçüm yapmak mantıksal
olarak mümkün değildir. Bunun yerine bilim insanları bir değişkenin tüm alanda
mekânsal olarak nasıl dağıldığını haritalamak için enterpolasyon yöntemini
kullanmayı tercih ederler. Birbirine yakın olan gözlem noktaları benzer
değerlere sahiptirler, ancak birbirinden uzak olan noktalar daha farklı
değerler taşırlar. Bu bilgi tahmin prosedüründe (enterpolasyon)
kullanılır. Burada bahsi geçen kriging yöntemleri de enterpolasyon
yöntemlerindendir. Kriging en uygun tahmin değerleri verir: bir değişkene ait
herhangi bir yerde en olası değeri üretir. Bu derleme çalışmasında
jeo-istatistikte en çok kullanılan kriging metotlarından Sıradan kriging,
Regresyon kriging ve Evrensel kriging yöntemlerine ait yöntemler anlatılmıştır.

Keywords

Jeoistatistik, Enterpolasyon, Sıradan kriging, Regresyon kriging, Evrensel kriging

Basic Kriging Methods in Geostatistics

Abstract

Measurements
of environmental, hydrological, agricultural and similar studies are based on
point observations over the Earth. Precipitation and temperature values are
measured from meteorological stations, soil characteristics are measured from
soil samples, and pollution of a lake is measured by taking samples from lake.
These are some examples from spatial point measurements. These variables can be
measured by taking samples from a limited number of locations or from certain
locations. However, it is logically impossible to measure a variable at all
parts of globe or on a field of certain size. Instead of this it is possible to
make some interpolation to map spatial distributions of that variable.
Observation locations which are close to each other tend to have similar
values, however the ones located farther apart from each other differ more. So
this knowledge is used in prediction procedure (interpolation).  Kriging which will be described here, is an
interpolation method. Kriging makes optimal predictions: it provides the most
likely value at any location of a variable. Methodologies of most commonly used
kriging methods in geostatistics; Ordinary kriging, Regression kriging and
Universal kriging have been described in this review work. 

Keywords

Geostatistics, Interpolation, Ordinary kriging, Regression kriging, Universal kriging

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