Gale Warning
Issued at: 5:00 PM TODAY , 17 October 2019
Gale Warning # 8
For: strong to gale force WINDS associated with the northeasterly surface windflow.

Gale Warning in PDF file



Weather Advisory
Issued at: 10:00 AM 2019 September 17
Weather Advisory in PDF file




General Flood Advisories - Regional
 General Flood Advisory issued as of 7 PM, 20 August 2018



Advisories


Monthly Climate Assessment and Outlook (July-August 2018)

Issued: 06 August 2018

Monthly Rainfall Forecast
RAINFALL FORECAST  (September 2018 - February 2019) 
UPDATED: 29 August 2018 (next update September 26, 2018)


Regional Rainfall Forecast
Issued: 29 August 2018
Valid for: September 2018 - February 2019
Farm Weather Forecast and Advisories
ISSUED: 8 AM,  FRIDAY,  MAY 24, 2019
VALID UNTIL: 8 AM,  SATURDAY, MAY 25
, 2019
FWFA:  N0. 19-144

Ten-Day Regional Agri-Weather Information
DEKAD NO. 15   MAY 21 - 31, 2019
PHILIPPINE AGRI-WEATHER FORECAST
The weather systems that will affect the whole country are the frontal system, easterlies, ridge of high pressure area, intertropical convergence zone (ITCZ) and low pressure area (LPA).

Seasonal Climate Outlook
Issued:  13 July 2018
FOR July - December 2018
PDF 




Astronomical Diary
Issue for October 2018
The October Orionids meteor shower will be active from October 17-25, 2017.




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Prisco D. Nilo
1995

A two-dimensional storm surge model with non-uniform grid system is developed and used to simulate four local storm surge occurrences and one well documented storm surge event in South Carolina, USA. The hydrodynamic equations are vertically integrated and the model considers the effects of surface stress, gradient in atmospheric and water pressure, bottom stress and coriolis acceleration. A Rankine-vortex typhoon model is used to generate the cyclonic wind field. In the computation of surface stress the bulk-aerodynamic parameterization is utilized. While the bottom stress is assumed to vary directly with the depth-averaged current and inversely with the depth of the fluid. The model also have provision for overland flooding and coastal drying. The movement of the coastal boundary is governed by the difference between the surge height and the elevation of the adjacent grid inland. A number of theoretical experiments are conducted to test the response of the model to changes in grid resolution and basin characteristics. Results show that the model is sensitive to grid resolution and that storm surge predominantly occurs in shallow continental shelves. It is also shown that bay-shaped basins attain higher surges compared to straight coastlines. Further, it is shown that inland slope controls the extent of inland flooding. Actual simulations were performed which include the 1912 storm surge in Sogod Bay, the 1975 storm surge in Tandag, the 1981 storm surge in Baler Bay, the 1994 case of Katring which generated an insignificant surge height in Lamon Bay, and the 1989 storm surge in South Carolina. The results of the simulations demonstrate that the model has shown modest skill to simulate the depth-averaged current driven by the intense tangential winds of typhoons and to predict reasonable surge heights. An operational procedure for storm surge forecasting is also presented in this study for future consideration.

Herman L. Ngohayon
1995

Upper tropospheric temperature anomalies (T250) and the horizontal Laplacian to the upper tropospheric temperature field (2T250) were determined from the radiances remotely sensed by the TIROS Operational Vertical Sounder (TOVS) on board a NOAA series (11 and 12) of polar orbiting satellite. A total of 88 cases from 18 tropical cyclones passing over the Philippine Region were monitored and surface pressure anomalies at 6-and 12-degree radius (P6 and P12) and maximum surface wind speed (Vmax) were obtained. Relating these data, a statistical model was developed to estimate the tropical cyclone intensity. Results showed excellent correlation with about 80% of the variations in Vmax was accounted for by T. No significant improvement in the coefficient of determination (r²) was achieved when ²T was regressed in linear form, exponentially and when both T and ²T were combined as predictors. The same trend is observed in the predictive equations for the pressure anomalies P6 and   P12. The dependent samples indicate standard errors of 10 kts and 8 hPa for maximum winds and surface pressure, respectively, which is comparable with the results obtained by Le Marshall et al. (1994) and Velden et al. (1991) for Western North Pacific tropical cyclones. The accuracy of the intensity estimates suggest that this method could be adopted operationally to supplement the Dvorak method of intensity estimation.