IASH General Assembly, Sapporo (Japan), 3-11 July 2003 TRANSACTIONS GLOBAL CHANGE--RISK ASSESSMENT AND REAL TIME HYDROLOGICAL FORECASTING OF FOREST CONFLAGRATIONS FOR WATER MANAGEMENT S. LOBANOV Far Eastern Regional Hydrometeorological Research Institute (FERHRI) 690600, 24, Fontannaya St., Vladivostok, Russia V. Kulik , CYPUM PTY LTD, P.O. Box 863, Canberra City, ACT, AUSTRALIA 2601 ABSTRACT The global change makes irrelevant many methods of risk assessment and forecasting. In particular, changing climate means a greater probability of forest conflagrations. This results in disabling of water supply watersheds and reservoir contamination. Old methods of meteorological forecasting of conflagrations will become less reliable, being based on correlations, obtained for a period of stable climate. EXISTING hydrological networks can be used for wild conflagration prediction. Runoff data allows the prediction of high fire danger earlier, with less overcaution, highlights the most dangerous watersheds and makes forecast more foolproof. In some cases hydroforecast improves the likelihood of prevention of a major disaster. This technique has certain DIFFERENCES from the standard meteorological methods: (1)It predicts bushfires not for an administrative or geographical region, but for a watershed-- so, a bushfire can be forecast for certain water supply reservoirs; (2) It allows forecast of the bushfire danger earlier and estimates of the amount of time available for active measures; (3) It is less overcautious, thus excluding most false alarm situations;(4) It is more accurate, simply because it uses hydrographical data, which is more representative than meteorological data;(5)It is more foolproof and less dependent on the errors of observations; (6) It depends less on the stochastical nature of summer rains and other meteorological elements.(7) It is simpler than any other method.There are two groups of PREDICTORS. (A) Early Predictors:(A1) Low flow; (A2) Change of the curvature of the recession curve from concave to convex (semi log paper);(A3) Accelerated recession. These early predictors can be used to estimate how many days there are before the critical fire danger starts (by an extrapolation of the recession curve). (B) Later Predictors: (B1) Stabilization of the runoff to a "zero flow" value; (B2) Steep rate of the recession after intermediate minor rains;(B3) Convex recession after intermediate rains.(B4) Abrupt stabilization of the runoff to "zero flow" several days after a minor rain. The manifestation of these late predictors means that the probability of a bushfire has increased dramatically. This method allows a forecast of the CRITICAL fire danger, when a bushfire is almost inevitable. Experimental risk assessment and real time forecast were successful for for water supply watersheds of Russia and Australia. Quite different tools may be used in any particular case, due to local customs, hardware and software. For example, in some cases a deviation from normal rainfall-runoff relationships (runoff-rainfall or water balance models) could be a good indicator. A conflagration is a very rare phenomenon and to collect sufficient amount of information for any development of the forecasting technique it is necessary simply to analyze more cases.We ask everybody who has in their disposal data on watersheds, affected by an intense bushfire, to try this simple technique, to develop it and to communicate their results.