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Current Research in Environmental Science and Ecology Letters(CRESEL)

ISSN: 2997-3694 | DOI: 10.33140/CRESEL

Research Article - (2025) Volume 2, Issue 1

Evaluation of the Change in Some Meteorological Variables Measured with the Automatic Station at the Yabu Meteorological Station, Cuba

Ricardo Oses Rodriguez * and Nancy Ruiz Cabrera
 
1Climate Department., Provincial Meteorological Center of Villa Clara, Cuba
 
*Corresponding Author: Ricardo Oses Rodriguez, Climate Department., Provincial Meteorological Center of Villa Clara, Cuba

Received Date: Apr 09, 2025 / Accepted Date: Nov 28, 2025 / Published Date: Dec 12, 2025

Copyright: ©©2025 Ricardo Osés Rodríguez, et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

Citation: Rodríguez, R. O., Cabrera, N. R. (2025). Evaluation of the Change in Some Meteorological Variables Measured with the Automatic Station at the Yabu Meteorological Station, Cuba. Curr Res Env Sci Eco Letters, 2(1), 01-04.

Abstract

For this work, the Regressive Objective Regression (ROR) methodology was used to model the three meteorological variables: extreme temperatures, maximum and minimum temperatures, and maximum rainfall within 24 hours. For this purpose, a step variable was designed, which takes a value of zero before the change, that is, before 2023, month 8, day 31, and takes a value of 1 after this date, which corresponds to the new automatic station. It can be seen that the model depends on temperatures and rainfall regressed over 11 years.Specifically, the new station represents a 1.39°C drop in minimum temperature. The trend is positive but very small and highly significant at 100%. For maximum temperature, the trend is positive but very small and highly significant at 100%. Similarly, for minimum temperature, the new station represents a 1.48°C drop. It is further confirmed that with the automatic station, both maximum and minimum temperatures are below what was measured at the previous station used by meteorologists. For maximum rainfall over 24 hours, the trend is positive but very small and highly significant. The new meteorological station reports a 2.9 mm decrease in rainfall. In the short term, the errors are smaller, and the impact of using the automatic station results in small and non-significant parameters. Therefore, it can be concluded that the average values from the Yabu station can be used, combined with the new data, at least in the short term.

Keywords

Change of Season, Extreme Temperatures, Trend, Maximum Rainfall in 24 Hours, Cuba

Introduction

Meteorological stations change location over time, and it becomes necessary to evaluate measurements under new conditions. The Yabu meteorological station ceased its usual operations in 2023, month 8, day 31, and from then on, data collection began using an automatic station. Therefore, it is necessary to evaluate the record- ings obtained with this new technique. Therefore, the objective of our work will be to assess this change in the main variables, such as extreme temperatures (maximum and minimum), as well as the maximum rainfall within 24 hours.

Materials and Methods

For this work, the Regressive Objective Regression Methodolo- gy (ROR) was used to model the three meteorological variables, namely, extreme temperatures, maximum, minimum, and maxi- mum rainfall in 24 hours [1-3]. For this purpose, a step variable was designed, which takes the value of zero before the change, that is, before 2023, month 8, day 31, and takes the value of 1 after this date, which corresponds to the new automatic station. It should be noted that gaps are observed in the automatic data collection due to the lack of electricity at some stages, which complicates the study. However, the results obtained were good.

Results and Discussion

The model for minimum temperature explains 99.3% of the vari- ability with an error of 2.3547. Fisher's F value is 92,717, signifi- cant at 100%. The model is as follows the Table 1 below. As can be seen, the model depends on temperatures regressed over 11 years.

In particular, Step.2023.08.31 represents a drop of 1.39°C with the use of the automatic station from that date onwards. It can be seen, for example, that the variable step4097 represents a drop of 4.4°C and is a case that has occurred in the station's history. The trend is positive but very small and highly significant at 100%.

Modelo

Coeficientes no estandarizados

Coeficientes estandarizados

t

Sig

B

Error estándar

Beta

1

DS

5,850

,162

,206

36,005

,000

DI

5,837

,162

,205

35,929

,000

Tendencia

2,743E-5

,000

,015

4,924

,000

Lag4015Tmin

,194

,014

,191

13,897

,000

Lag4016Tmin

,040

,015

,039

2,587

,010

Lag4018Tmin

,200

,011

,197

18,583

,000

Lag4029Tmin

,268

,009

,265

31,026

,000

Step.2023.08.31

-1,387

,240

-,006

-5,786

,000

Step4097

-4,416

2,355

-,002

-1,875

,061

Step4043

,100

2,357

,000

,043

,966

a. Variable dependiente: Tmin

b. Regresión lineal a través del origen

Table 1: Co-efficientsa, b

In the case of the Maximum Temperature, Table 2., the explained variance is 99.7 with an error of 2.37, Fisher's F is 210068 signif- icant at 100%. The trend is positive but very small and highly sig- nificant at 100%, as in the Minimum Temperature. The new station represents a drop of 1.48 ºC, then it is corroborated that with the automatic station both the maximums and minimums are below what were measured with the previous station where meteorolo- gists were used to measure.

Modelo

Coeficientes no estandarizados

Coeficientes estandarizados

t

Sig.

B

Error estándar

Beta

1

DS

8,694

,262

,203

33,211

,000

 

DI

8,686

,262

,203

33,178

,000

 

Tendencia

3,171E-5

,000

,012

5,644

,000

 

Lag4015Tmax

,164

,012

,163

13,302

,000

 

Lag4016Tmax

,096

,013

,095

7,261

,000

 

Lag4018Tmax

,218

,010

,216

22,048

,000

 

Lag4029Tmax

,229

,009

,228

26,552

,000

 

Step.2023.08.31

-1,478

,241

-,004

-6,119

,000

 

Step4097

-8,969

2,375

-,003

-3,777

,000

 

Step4043

-10,707

2,375

-,003

-4,508

,000

a. Variable dependiente: Tmax

b. Regresión lineal a través del origen

Table 2: Coeficientesa, b

For the 24-hour maximum rainfall (Table 3), a model was obtained that explains 50.7% of the rainfall with an error of 9.7 mm. Fisher's F is 143, significant at 100%. The trend is positive but very small and highly significant. The new weather station reports a 2.9 mm decrease in rainfall.

Modelo

Coeficientes no estandarizados

Coeficientes estandarizados

t

Sig.

B

Error estándar

Beta

 

DS

1,729

,275

,109

6,289

,000

DI

2,077

,275

,131

7,549

,000

Tendencia

7,860E-5

,000

,079

3,466

,001

Lag4015r24h

,026

,008

,025

3,051

,002

Lag4016r24h

,028

,008

,027

3,286

,001

Lag4017r24h

,029

,008

,029

3,461

,001

Lag4018r24h

,022

,008

,021

2,579

,010

Lag4020r24h

,033

,008

,032

4,003

,000

Lag4029r24h

,032

,008

,032

3,924

,000

Lag3650r24h

,032

,008

,031

3,877

,000

Step.2023.08.31

-2,938

,885

-,026

-3,321

,001

Step7937

236,283

9,697

,186

24,366

,000

Step8322

122,317

9,686

,096

12,628

,000

Step8594

72,740

9,686

,057

7,510

,000

Step8685

55,601

9,686

,044

5,740

,000

Step8885

63,073

9,686

,050

6,512

,000

Step11342

107,126

9,686

,084

11,060

,000

Step11564

61,137

9,688

,048

6,310

,000

Step11574

85,584

9,686

,067

8,836

,000

Step12205

62,868

9,690

,049

6,488

,000

Step12535

84,651

9,700

,066

8,727

,000

Step12578

117,940

9,688

,093

12,174

,000

Step12927

90,766

9,693

,071

9,364

,000

Step12932

61,951

9,690

,049

6,393

,000

Step13082

104,293

9,686

,082

10,767

,000

Step13180

76,387

9,686

,060

7,886

,000

Step4169

95,651

9,698

,075

9,863

,000

Step4301

94,806

9,687

,074

9,787

,000

Step7230

160,427

9,686

,126

16,563

,000

Step8350

93,509

9,686

,073

9,654

,000

Step10416

162,450

9,686

,128

16,772

,000

a. Variable dependiente: r 24h

b. Regresión lineal a través del origen

Table 3: Coeficientesa, b

The model for these variables is very long-term (11 years in ad- vance). It was analyzed that the short-term model results in small- er errors, and the impact of using the automatic station results in small, non-significant parameters. Therefore, it can be concluded that the mean values from the Yabu station can be used, combined with the new data, at least in the short term.

Conclusions

• As can be seen, the model depends on temperatures and precipitation returned over 11 years. In particular, the new automatic station represents a 1.39°C drop in minimum temperature. The trend is positive but very small and highly significant at 100%.

• In the case of maximum temperature, the trend is positive but very small and highly significant at 100%, as is the case with minimum temperature. The new station represents a drop of 1.48°C. It is then confirmed that with the automatic station, both the maximum and minimum temperatures are below what was measured with the previous station used by meteorologists.

• For the maximum rainfall over 24 hours, the trend is positive but very small and highly significant. The new meteorological station reports a 2.9 mm decrease in rainfall.

• In the short term, the errors are smaller, and the impact of using the automatic station results in small and non-significant parameters. Therefore, it can be concluded that the average values from the Yabu station can be used, combined with the new data, at least in the short term.

References

  1. González, F. M. W. (2022). Methodology of The Objective Regressive Regression In Function of The Prognosis For Deaths, Critical, Severe, Confirmed And New Cases ofCovid-19 In Santa Clara Municipality and Cuba. Research Review, 3(01), 604-612.
  2. Osés, R.R., Fimia, D.R., Osés, L.C., y Jerez, P.L.E. (2022b).Forecasts for deaths, critical cases, serious, confirmed and new cases of COVID-19 in the municipality of Santa Clara and Cuba using the Regressive Objective Regression methodology. UO Medical Affairs. 1(1), 28-39.
  3. Rodríguez, R. O., Fimia-Duarte, R., del Valle Laveaga, D., Martin, M. O., Cabrera, N. R., Ferrer, Y. Z., ... & González, F. M. W. (2022). Mathematical Modeling and Its Applicability from Natural Disasters to Human Health.