diff --git a/pyTMD/arguments.py b/pyTMD/arguments.py
index b0bf032d..5202c5a2 100755
--- a/pyTMD/arguments.py
+++ b/pyTMD/arguments.py
@@ -1420,7 +1420,7 @@ def _constituent_parameters(c: str, **kwargs):
     _omega = np.array([1.405189e-04, 1.454441e-04, 7.292117e-05, 6.759774e-05,
         1.378797e-04, 7.252295e-05, 1.458423e-04, 6.495854e-05, 1.352405e-04,
         1.355937e-04, 1.382329e-04, 1.431581e-04, 1.452450e-04, 7.556036e-05,
-        7.028195e-05, 7.824458e-05, 6.531174e-05, 0.053234e-04, 0.026392e-04,
+        7.025945e-05, 7.824458e-05, 6.531174e-05, 0.053234e-04, 0.026392e-04,
         0.003982e-04, 2.810377e-04, 2.859630e-04, 2.783984e-04, 4.215566e-04,
         5.620755e-04, 2.134402e-04, 4.363323e-04, 1.503693e-04, 2.081166e-04,
         4.925200e-06, 1.990970e-07, 7.962619e-06, 6.231934e-05])
@@ -1429,10 +1429,10 @@ def _constituent_parameters(c: str, **kwargs):
     # the forcing for that constituent is zero on the Greenwich meridian
     _phase = np.array([1.731557546, 0.000000000, 0.173003674, 1.558553872,
         6.050721243, 6.110181633, 3.487600001, 5.877717569, 4.086699633,
-        3.463115091, 5.427136701, 0.553986502, 0.052841931, 2.137025284,
-        2.436575100, 1.929046130, 5.254133027, 1.756042456, 1.964021610,
+        3.463115091, 5.427136701, 0.553986502, 0.050398470, 2.137025284,
+        2.436575000, 1.929046130, 5.254133027, 1.756042456, 1.964021610,
         3.487600001, 3.463115091, 1.731557546, 1.499093481, 5.194672637,
-        6.926230184, 1.904561220, 0.000000000, 4.551627762, 3.809122439,
+        6.926230184, 1.904561220, 0.000000000, 4.551627762, 3.290111417,
         4.551627762, 6.232786837, 3.720064066, 3.91369596])
     # amplitudes of equilibrium tide in meters
     # _amplitude = np.array([0.242334,0.112743,0.141565,0.100661,0.046397,
diff --git a/test/test_arguments.py b/test/test_arguments.py
index 67c7c251..e5661138 100644
--- a/test/test_arguments.py
+++ b/test/test_arguments.py
@@ -679,10 +679,10 @@ def test_parameters():
     """
     Test constituent parameter values
     """
-    # parametrized constituents (sans m1 and 2mk3)
+    # parametrized constituents
     cindex = ['m2', 's2', 'k1', 'o1', 'n2', 'p1', 'k2', 'q1', '2n2', 'mu2',
-        'nu2', 'l2', 'j1', 'oo1', 'rho1', 'mf', 'mm', 'ssa',
-        'm4', 'ms4', 'mn4', 'm6', 'm8', 'mk3', 's6', '2sm2', 
+        'nu2', 'l2', 't2', 'j1', 'm1', 'oo1', 'rho1', 'mf', 'mm', 'ssa',
+        'm4', 'ms4', 'mn4', 'm6', 'm8', 'mk3', 's6', '2sm2', '2mk3',
         'msf', 'sa', 'mt', '2q1']
     # number of days between MJD and the tide epoch (1992-01-01T00:00:00)
     MJD = np.atleast_1d(48622.0)
@@ -703,13 +703,14 @@ def test_parameters():
     for i, c in enumerate(cindex):
         # get constituent parameters
         amp, ph, omega, alpha, species = _constituent_parameters(c)
+        # convert phase to degrees
+        phase = np.mod(180.0*ph/np.pi, 360.0)
         # check species
         cartwright = doodson_number(c, formalism='Cartwright')
         assert species == cartwright[0]
         # check frequency calculation
         assert np.isclose(omega, omegas[i])
         # assert phase calculation
-        phase = np.mod(180.0*ph/np.pi, 360.0)
         assert np.isclose(phase, G[0,i])
         
 def test_doodson():