286 9 Dressing via nonlocal Riemann–Hilbert problem
Finally, the boundary condition (9.13) gives
∞
−∞
dxΦ
j
(x)=−πi. (9.43)
9.1.4 RH problem
Now we have all ingredients to formulate the RH problem for the BO equation.
Indeed, because the Green function G
+
is analytic in the upper half k-plane, it
follows from the theory of Fredholm integral equations [425] that the solution
M
+
(x, k) is analytic in the same region as well, except for possible poles
at isolated p oints k
j
, where nontrivial solutions of the homogeneous integral
equation exist. The same analytic properties but in the lower half plane are
inherent to the eigenfunction M
−
(x, k). As regards N
±
, they cannot in general
be continued off the real k-a xi s because of the exponent e
ikx
. On the other
hand, there is a differential connection (9.23) between the functions N
−
and
M
−
. This fact enables us, by means of (9.18), (9.23), and (9.37), to p ose the
RH problem of the form
M
+
(x, k)=M
−
(x, k)+
β(k)
2πi
k
0
dk
′
k
′
β
∗
(k
′
)e
−ik
′
x
M
−
(x, k
′
). (9.44)
The normalization of the RH problem (9.44) is given by
M
+
(x, k) → 1atk →∞. (9.45)
It should be noted that the RH problem (9.44) is essentially distinct from
the RH problems we dealt with in the preceding chapter. Namely, t he RH
problem (9.44) is nonlocal in that stems from the nonlocality of the BO equa-
tion. The spectral data of the RH problem (9.44) are determined by the set
{β(k),k > 0; k
j
, Reγ
j
,j =1,...,N}.
2
As usual, we can regularize the RH
problem and represent its solutions M
+
and M
−
as
M
+
(x, k)=1−i
N
j=1
(k −k
j
)
−1
Φ
j
(x)+ m
+
(x, k),m
+
(x, k →∞)=0, (9.46)
M
−
(x, k)=1−i
N
j=1
(k−k
j
)
−1
Φ
j
(x)+m
−
(x, k),m
−
(x, k →∞)=0, (9.47)
where the holomorphic functions m
±
(x, k)are(+)and(–)functionswith
respect to x, respectively. The fact that the spectral problem (9.2) allows
only simple poles was proved in [362].
2
It will be shown later that Imγ
j
canbeexpressedintermsofk
j
.