The transient behaviour, i.e., the growth process of storm surges and other forced long waves is analysed through analytical solution to the small amplitude I D case. The growing long wave is modelled as the superposition of the asymptotic, steady forced solution and a pair of free waves which cancel it at time zero and subsequently move away from it, while perhaps decaying. This approach leads to useful new qualitative insights. First of all, it is clear that the timescale for the growth of a surge is L-surge/vertical bar root gh - c vertical bar, i.e., its length divided by the speed difference between the forcing and the free waves. Secondly, the surge landfall scenarios with fast versus slow moving low pressure systems are similar altho...
In the open ocean the formation of large waves is non-linear. This non-linearity modifies the shape ...
The 2D‐parametric model suggested in the companion paper is used to simulate waves under Tropical Cy...
A fully consistent 2D parametric model of wave development under spatially and/or time varying winds...
The highly transient initial shapes of 1D forced long waves are described in analogy with the swingi...
We obtain an analytic representation for the profile of the surge wave in the sea, due to a tropical...
Long period surface ocean waves generated by atmospheric disturbances represent a worldwide coastal ...
The observed trend of peak storm surge eta(max) increasing with storm size R-max, roughly as eta(max...
Coastal areas around the world are frequently attacked by various types of storms, threatening human...
The local linear stability of forced, stationary long waves produced by topography or potential vort...
Debris flows are often described as a succession of surges, which are characterized by enhanced peak...
A Storm surge is an offshore rise of water caused primarily by high winds pushing on the ocean's sur...
The evolution of long waves generated by a pressure disturbance acting on an initially unperturbed f...
International audienceA model is developed to explain the observation made in several laboratory exp...
International audienceStorms usually induce a surge that causes the water level to reach a higher po...
Storm surges are often characterized in terms of magnitude, duration and frequency. Here, we propose...
In the open ocean the formation of large waves is non-linear. This non-linearity modifies the shape ...
The 2D‐parametric model suggested in the companion paper is used to simulate waves under Tropical Cy...
A fully consistent 2D parametric model of wave development under spatially and/or time varying winds...
The highly transient initial shapes of 1D forced long waves are described in analogy with the swingi...
We obtain an analytic representation for the profile of the surge wave in the sea, due to a tropical...
Long period surface ocean waves generated by atmospheric disturbances represent a worldwide coastal ...
The observed trend of peak storm surge eta(max) increasing with storm size R-max, roughly as eta(max...
Coastal areas around the world are frequently attacked by various types of storms, threatening human...
The local linear stability of forced, stationary long waves produced by topography or potential vort...
Debris flows are often described as a succession of surges, which are characterized by enhanced peak...
A Storm surge is an offshore rise of water caused primarily by high winds pushing on the ocean's sur...
The evolution of long waves generated by a pressure disturbance acting on an initially unperturbed f...
International audienceA model is developed to explain the observation made in several laboratory exp...
International audienceStorms usually induce a surge that causes the water level to reach a higher po...
Storm surges are often characterized in terms of magnitude, duration and frequency. Here, we propose...
In the open ocean the formation of large waves is non-linear. This non-linearity modifies the shape ...
The 2D‐parametric model suggested in the companion paper is used to simulate waves under Tropical Cy...
A fully consistent 2D parametric model of wave development under spatially and/or time varying winds...